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国後島の金鉱床の現状: 北方領土の地下資源について
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Stratiform arkose-hosted and shale-hosted copper Zambian copperbelt.
Data from the synthesis of ore deposits.
Data plotted and diagrams prepared by W.
Cu-Mo Cu -Au Mo -W Skarn Mineral deposits formed by replacement of limestone by ore and calc-silicateminerals, usually adjacent to a felsic レンジャーはどうやってスペルスロットを取り戻すのですか? granitic intrusive body.
Hypothermal - Cu -Au Mesothermal - Cu-Pb-Zn-Ag-Au Epithermal - Au-Ag -Hg Mississippi Valley Named for the region where they were first described, these deposits formed within porous carbonate rocks limestone reefs or caves.
They are Pb-Zn deposits with low Ag values.
Syngenetic Volcanic Massive Sulphide VMS These deposits formed as massive over 60% sulphide lens-like accumulations on or near the sea floor in association with volcanic activity.
Pb-Zn-Ag Ba Magmatic- layered mafic intrusion During the crystallization of a magma, usually mafic or ultramafic, heavy, metal-rich liquids settle and accumulate at specific sites, often at the base, within the intrusion.
PGM Platinum group metals Chromite Ni-Cu -PGM Placer Formed within sediments by the concentration of heavy resistant minerals Au diamond, cassiterite by stream or wave action.
Iceland, in something カジノカルガリー求人 are north Atlantic, 金鉱床 the tip of one part of this mountain range.
Volcanogenic massive sulfide VMS deposits described in the text are an example of mineral deposits that form on the sea floor.
Also shown are convergent plate boundaries where an oceanic plate is here subducted beneath a continental tectonic plate forming folded and faulted mountains orogen and volcanoes.
The subduction of oceanic tectonic plates is accompanied by strong earthquakes and the generation and movement of tmagma molten rock and hydrothermal fluids that form a variety of mineral deposits, including porphyry copper deposits and associated gold and silver veins and polymetallic replacement deposits and associated gold and silver veins and polymetallic replacement deposits described in this report.
Continental rift zones are areas where the crust is stretched extended forming linear depressions characterized by faults, volcanoes, sedimentary basins, and a source of mineral deposit types including sediment-hosted sedex lead-sinc, sediment-hosted copper, and evaporite deposits.
See text for further discussion.
Modified from Kious and Tilling 1996.
Compositional fields of arc volcanic rocks, high-temperature volcanic fumaroles, magmatic-hydrothermal fluids, and geothermal fluids are shown, as discussed by Einaudi et al.
Simplified from Einaudi et al.
Schematic sections of end-member volcanotectonic settings and associated epithermal and related mineralization types.
Calc-alkaline volcanic arc with neutral to mildly extensional stress state 金鉱床 relationships between high- and intermediate-sulfidation epithermal and porphyry deposits note that the complete spectrum need not be present everywhere.
Later, less acidic intermediate-sulfidation fluid gives rise to ntermediate-sulfidation mineralization, both djacent to and distal from the advanced argillic lithocap.
Where the intermediate-sulfidation fluid flows through the leached lithocap environment, it evolves to a high-sulfidation fluid Einaudi et al.
The high-sulfidation fluid may 金鉱床 back to intermediate-sulfidation stability during late stages, supported by paragenetic relationships and lateral transitions of high- to intermediate-sulfidation mineralogy.
See text for details.
Rift with bimodal volcanism and low-sulfidation deposits.
Henley and Ellis, 1983; Giggenbach, 1992; John, 2001.
Structure and processes beneath an 金鉱床 island arc sources: Tatsumi and Eggins, 1995; Schmidt and Poli, 1998; Winter, 2001; Poli and Schmidt, 2002; Fumagalli and Poli, 2005.
Primary hydrous basaltic arc magmas are derived from partial melting of the metasomatized asthenospheric mantle wedge.
Mineral zones shown in the 金鉱床 plate indicate lower limits of stability of hydrous phases in the basaltic oceanic crust and peridotitic mantle lithosphere.
Evolved, less dense, andesitic magmas rise into the mid-to-upper crust where they pool at their new level of neutral buoyancy to form batholithic complexes.
Along with volcanic structures, porphyry and epithermal deposits may form at shallower levels above these batholithic complexes where exsolved magmatic fluids ascend, cool, and interact with near-surface upper crustal rocks.
Modified fromRichards 2003, 2005 ; sources: Hildreth andMoorbath 1988 ,Winter 2001Annen et al.
Post-subduction tectonic environments conducive to the formation of porphyry and epithermal deposits by remobilization of previously subduction-modified lithosphere modified from Richards, 2009.
Such magmas may remobilize Au as well as Cu±Mo left behind in residual sulfide phases by arc magmatism, leading to the potential formation of porphyry Cu±Au±Mo and alkalic-type epithermal Au deposits.
See text for discussion.
Schematic cross-section through a typical coupled arc batholith.
Also shown are the thermal structure, fluid flow pathways and characteristics during the main stage of hydrothermal activity, and overlapping hydrothermal alteration zones.
Propylitic alteration by circulating heated groundwaters can be assumed to affect all the supracrustal rocks in the field of view, with greatest intensity epidote, actinolite close to the intrusions, fading to background distally.
Modified from Richards 2005 ; sources: Sillitoe 1973, 2010Dilles 1987Shinohara and Hedenquist 1997Hedenquist et al.
Also shown are the ages of the link deposits and etallogenic provinces mentioned in the book.
Base metals include Cu, Pb, and Zn filled dotsand precious metals comprise Au, 宝石ゲーム, and Hg open circles.
The numbers next to individual points or ranges refer to average concentrations or ranges in a variety of different situations, and are all after Seward and Barnes 1997.
The length of each histogram bar is an estimate of the proportion of ore formed over a 50 million year interval relative to the global resource for that deposit type.
Periods of supercontinent amalgamation are shown as Pangea, Rodinia, and Nena, with decreasing levels of confidence further back in time.
The diagram is originally after Meyer 1988 and modified after Barley and Groves 1992.
Phanerozoic porphyry belts, porphyry deposits, and representative porphyry 金鉱床 deposits summarized in Appendix 2 red labels.
Modified from Seedorff and others 2005, their Fig.
General setting of porphyry copper and associated deposit types modified from Sillitoe and Bonham, 1990.
Detailed descriptions are provided in the text modified after the models of Candela and Holland, 1984; 金鉱床 Strong, 1988; Candela, 1992.
Location of explored Nb- and REE-carbonatite deposits included in the database and grade and tonnage models.
Volcanogenic massive sulfide deposit subtypes mentioned in this paper.
World map showing the distribution of volcanogenic massive sulfide deposit subtypes.
Footwall rocks may consist of a sheeted dyke complex and the associated volcanics are often pillowed and have a tholeiitic composition.
After Hutchinson and Searle 1971.
Associated volcanics may be intermediate or felsic in composition and a closer lateral link to chemical and epiclastic sediments is often apparent.
The lens of massive sulfide ore formed on the ocean floor, underlain by a stockwork zone of disseminated sulfides and intensely 1アップスロット無料ダウンロード volcanic rock, is typical of VMS deposits in general after Large, 1992.
Both diagrams after Large 1992.
Global distribution of Mississippi Valley-Type lead-zinc deposits and districts.
Deposits are associated with broad redox boundaries and feature sodic alteration of source rocks and potassic alteration of host rocks.
A genetic link between high-sulfidation epithermal Au?
Cu and sub-volcanic porphyry type Cu?
Au deposits is also suggested after Hedenquist et al.
The diagram is relevant to both Chapters 2 and 3, and is modified after Skinner 1997.
Ficklin plot of the sum of the base metals Cd, Co, Cu, Ni, Pb, and Zn versus pH illustrating the variation of mine drainage chemistry as a function of the geologic characteristics type of specific mineral deposits.
Modified from Plumlee and Nash 1995and Plumlee 1999.

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沖縄で発見 最大規模の鉱物資源の“熱水鉱床”(15/01/28)

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カテゴリー:私たちのこと. 2013.04.11. 露出する金鉱床. 金鉱脈が目の前に. 聞いてびっくり。いつも目にする道路際の崖にそれはありました。一本の白い岩の筋(地層)が頂上めがけて斜めに走っています。金工芸も発達していたインカにちなみ「インカの階段」と.


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Stratiform arkose-hosted and shale-hosted copper Please click for source copperbelt.
Data from the synthesis of ore deposits.
Data plotted and diagrams prepared by W.
Cu-Mo Cu -Au Mo -W Skarn Mineral deposits formed by replacement of limestone by ore and calc-silicateminerals, usually adjacent to a felsic or granitic intrusive body.
Hypothermal - Cu -Au Mesothermal - Cu-Pb-Zn-Ag-Au Epithermal - Au-Ag -Hg Mississippi Valley Continue reading for the region where they 金鉱床 first described, these deposits formed within porous carbonate rocks limestone reefs or caves.
They are Pb-Zn deposits with low Ag values.
Syngenetic Volcanic Massive Sulphide VMS These deposits formed as massive over 60% sulphide lens-like accumulations on or near the sea floor in association with volcanic activity.
Pb-Zn-Ag Ba Magmatic- layered mafic intrusion During the crystallization of a magma, usually mafic or ultramafic, heavy, metal-rich liquids settle and accumulate at specific sites, often at the base, within the intrusion.
PGM Platinum group metals Chromite Ni-Cu -PGM Placer Formed within sediments by the concentration of heavy resistant minerals Au diamond, cassiterite by stream or wave action.
Iceland, in the north Atlantic, is the tip of one part of this mountain range.
Volcanogenic massive sulfide VMS deposits described in the text are an example of mineral deposits that form on the sea floor.
Also shown are convergent plate boundaries where an oceanic plate is being subducted beneath a continental tectonic plate forming folded and faulted mountains orogen and volcanoes.
The subduction of oceanic tectonic plates is accompanied by strong earthquakes and the generation and movement of tmagma molten rock and hydrothermal fluids that form a variety of mineral deposits, properties ヒューゴゲームオンライン agree porphyry copper deposits and associated gold and silver veins and polymetallic replacement deposits and associated gold and silver veins and polymetallic replacement deposits described in this report.
Continental rift zones are areas where the crust is stretched extended forming linear depressions characterized by faults, volcanoes, sedimentary basins, and a variety of mineral deposit types including sediment-hosted sedex lead-sinc, sediment-hosted copper, and evaporite deposits.
See text for further discussion.
Modified from Kious and Tilling 1996.
Compositional fields of arc volcanic rocks, high-temperature volcanic go here, magmatic-hydrothermal fluids, and geothermal fluids are shown, as discussed by Einaudi et al.
Simplified from Einaudi et al.
Schematic sections of end-member volcanotectonic settings and associated epithermal and related mineralization types.
Calc-alkaline volcanic arc 衝撃波プレーヤーゲーム3 d neutral to mildly extensional stress state showing relationships between high- and intermediate-sulfidation epithermal and porphyry deposits note that the complete spectrum need not be present everywhere.
Where the intermediate-sulfidation fluid flows through the leached lithocap environment, 金鉱床 evolves to a high-sulfidation fluid Einaudi et al.
The high-sulfidation fluid may evolve back to intermediate-sulfidation stability during late stages, supported by paragenetic relationships and lateral transitions of high- to intermediate-sulfidation mineralogy.
See text for details.
Rift with bimodal volcanism and low-sulfidation deposits.
Henley and Ellis, 1983; Giggenbach, 1992; John, 2001.
Structure and processes beneath an oceanic island arc sources: Tatsumi and Eggins, 1995; Schmidt and Poli, 1998; Winter, 2001; Poli and Schmidt, 2002; Fumagalli and Poli, 2005.
Primary hydrous basaltic arc magmas are derived from partial 金鉱床 of the metasomatized asthenospheric mantle wedge.
Mineral zones shown in the subducting plate indicate lower limits of stability of hydrous phases in the basaltic oceanic crust and peridotitic mantle lithosphere.
Evolved, less dense, andesitic magmas rise into the mid-to-upper crust where they pool at their new level of neutral buoyancy to form batholithic complexes.
Along with volcanic structures, porphyry and epithermal deposits may form at shallower levels above these batholithic complexes where exsolved magmatic fluids ascend, cool, and interact with near-surface upper crustal rocks.
Modified fromRichards 2003, 2005 ; sources: Hildreth andMoorbath 1988 ,Winter 2001Annen et al.
Post-subduction tectonic environments conducive to the formation of porphyry and epithermal deposits by remobilization of previously subduction-modified lithosphere modified from Richards, 2009.
Such magmas may remobilize Au as well as Cu±Mo left behind in residual sulfide phases by arc magmatism, leading to the potential formation of porphyry Cu±Au±Mo and alkalic-type epithermal Au deposits.
See text for discussion.
Schematic cross-section through a typical coupled arc batholith.
Also shown are the thermal structure, fluid flow pathways and characteristics during the main stage of hydrothermal activity, and overlapping hydrothermal alteration zones.
Propylitic alteration by circulating heated groundwaters can be assumed to affect all the supracrustal rocks in the field of view, with greatest intensity epidote, actinolite close to the intrusions, fading to background distally.
Modified from Richards 2005 ; sources: Sillitoe 1973, 2010Dilles 1987Shinohara and Hedenquist 1997Hedenquist et al.
Also shown are the ages of the various deposits and etallogenic provinces mentioned in the book.
Base metals include Cu, Pb, and Zn filled dotsand precious ゲンティンカジノグラスゴーポーカースケジュール comprise Au, Ag, and Hg open can 新しい素晴らしいゲームはクリケットをダウンロード opinion />The numbers next to individual points or ranges refer to average concentrations or ranges in a variety of different situations, and are all after Seward and Barnes 1997.
The length of each histogram bar is an estimate of the proportion of ore formed over a 50 million year interval relative to the global resource for that deposit type.
Periods of supercontinent amalgamation are shown as Pangea, Rodinia, and Nena, with decreasing levels of confidence further back in time.
The diagram is originally after Meyer 1988 and modified after Barley and Groves 1992.
Phanerozoic porphyry belts, porphyry deposits, and representative porphyry copper deposits summarized in Appendix 2 red labels.
Modified from Seedorff and others 2005, their Fig.
General setting of porphyry copper and associated deposit types modified from Sillitoe and Bonham, 1990.
Detailed descriptions are provided in the text modified after the models of Candela and Holland, 1984; 1986; Strong, 1988; Candela, 1992.
Location of explored Nb- and REE-carbonatite deposits included in the database and grade and tonnage models.
Volcanogenic massive sulfide deposit subtypes mentioned in this paper.
World map showing the distribution of volcanogenic massive sulfide deposit subtypes.
Footwall rocks may consist of a sheeted dyke complex and the associated volcanics are often pillowed and have a tholeiitic composition.
After Hutchinson and Searle 1971.
Associated volcanics may be intermediate or felsic in composition and a closer lateral link to chemical and epiclastic sediments is often apparent.
The lens of massive sulfide ore formed on the ocean floor, underlain by a stockwork zone of disseminated sulfides and intensely altered volcanic rock, is typical of VMS deposits in general after Large, 1992.
Both diagrams after Large 1992.
Global distribution of Mississippi Valley-Type lead-zinc deposits and districts.
Deposits are associated with broad redox boundaries and feature sodic alteration of source rocks and potassic alteration of host rocks.
A genetic link between high-sulfidation epithermal Au?
Cu and sub-volcanic porphyry type Cu?
Au deposits is also suggested after Hedenquist et al.
The diagram is relevant to both Chapters 2 and 3, and is modified after Skinner 1997.
Ficklin plot of the sum of the base metals Cd, Co, Cu, Ni, Pb, and Zn versus pH illustrating the variation of mine drainage chemistry as a function of the geologic characteristics type 金鉱床 specific mineral 金鉱床 />Modified from Plumlee and Nash 1995and Plumlee 金鉱床.

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熱水性金鉱床を形成する金の吸着࣭沈殿メカࢽズムの解明. Investigation of Gold Adsorption/Precipitation Mechanism. During the Formation of Hydrothermal Gold Deposit. 米津 幸太郎 a, 大橋 弘範 b, 川本 大祐 c, 安東 宏晃 c,. 本間 徹生 d, 横山 拓史.


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イスラエル富豪のコンゴの金鉱床、埋蔵量は「世界クラス」か - Bloomberg
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罪人の金鉱床 · 「罪人の金鉱床」に関する記事 「罪人の金鉱床」に関する商品. 罪人の金鉱床のイラストやマンガは1件投稿されています。罪人の金鉱床と一緒に付けられている主なタグには茨華仙、なにこれかっこいい、茨歌仙、茨木華扇などがあります。


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タイトル, 鹿児島県大口鉱山の金鉱床に伴う粘土鉱物. 著者, 横溝 宏佳. 出版年, 1969-03. 対象利用者, 一般. 資料の種別, 記事・論文. 掲載誌情報(ISSN形式), 03858278. 掲載誌情報(ISSNL形式), 03858278. 掲載誌情報(URI形式).


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明石の改修工廠早見表 | Simplified Chart for Akashi
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佐渡金山の金は火山活動によって濃集し、岩石中の割れ目を満たした鉱脈の中に銀や銅の鉱物とともに産出します。 このような金を山金(やまきん)と呼びます。 一方、古代エジプトやメソポタミアの金は砂金として採取されたもので、この様な鉱床を漂砂鉱床と.


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浜頓別町 砂金豆知識
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Stratiform arkose-hosted and shale-hosted copper Zambian copperbelt.
Data from the synthesis of ore deposits.
Data plotted and diagrams prepared by W.
Cu-Mo Cu -Au Mo -W Skarn Mineral deposits formed by replacement of limestone by ore and calc-silicateminerals, usually adjacent to a felsic or granitic intrusive body.
Hypothermal - Cu -Au Mesothermal - Cu-Pb-Zn-Ag-Au Epithermal - Au-Ag -Hg Mississippi Valley Named for the region where they were first described, these deposits formed within porous carbonate rocks limestone reefs or caves.
They are Pb-Zn deposits with low Ag source />Syngenetic Volcanic Massive Sulphide VMS These deposits formed as massive over 60% sulphide lens-like accumulations on or near the sea floor in association continue reading volcanic activity.
Pb-Zn-Ag Ba Magmatic- layered mafic intrusion During the crystallization of a magma, usually mafic here ultramafic, heavy, metal-rich liquids settle and accumulate at specific sites, often at the base, within the intrusion.
PGM Platinum group metals Chromite Ni-Cu -PGM Placer Formed within sediments by the concentration of heavy resistant minerals Au diamond, cassiterite by stream or wave action.
Iceland, in the north Atlantic, is the tip of one part of this mountain range.
Volcanogenic massive sulfide VMS deposits described in the text are an example of mineral deposits that form on the sea floor.
Also shown are convergent plate boundaries where an oceanic plate is being subducted beneath a continental tectonic plate forming folded and faulted mountains orogen and volcanoes.
The subduction of oceanic tectonic plates is accompanied by strong earthquakes and the generation and movement of tmagma molten rock 金鉱床 hydrothermal fluids that form a variety of mineral deposits, including porphyry copper deposits and associated gold and silver veins and polymetallic replacement deposits and 金鉱床 gold and silver veins and polymetallic replacement deposits described in this report.
Continental rift zones are areas where the crust is stretched extended forming linear depressions characterized by faults, volcanoes, sedimentary basins, and a variety of mineral deposit types including sediment-hosted sedex lead-sinc, sediment-hosted copper, and evaporite deposits.
See text for further discussion.
Modified from Kious and Tilling 1996.
Compositional fields of arc volcanic rocks, high-temperature volcanic fumaroles, magmatic-hydrothermal fluids, and geothermal fluids are shown, as discussed by Einaudi et al.
Simplified from Einaudi et al.
Schematic sections of end-member volcanotectonic settings and associated epithermal and related mineralization types.
Calc-alkaline volcanic arc with neutral to mildly extensional stress state showing 金鉱床 between high- and intermediate-sulfidation epithermal and porphyry deposits note that the complete spectrum need not be present everywhere.
Later, less acidic intermediate-sulfidation fluid gives rise to ntermediate-sulfidation mineralization, both djacent to and distal from the advanced argillic lithocap.
Where the intermediate-sulfidation fluid flows through the leached lithocap environment, it evolves to a high-sulfidation fluid Einaudi et al.
The high-sulfidation fluid may evolve back to intermediate-sulfidation stability during late stages, supported by paragenetic relationships and lateral transitions of high- to intermediate-sulfidation mineralogy.
See text for details.
Rift with bimodal volcanism and low-sulfidation deposits.
Henley and Ellis, 1983; Giggenbach, 1992; John, 2001.
Structure and processes beneath an oceanic island arc sources: Tatsumi and Eggins, 1995; Schmidt and Poli, 1998; Winter, 2001; Poli and Schmidt, 2002; Fumagalli and Poli, 2005.
Primary hydrous basaltic arc magmas are derived from partial melting of the metasomatized asthenospheric read article wedge.
Mineral zones shown in the subducting plate indicate lower limits of stability of hydrous phases in the basaltic oceanic crust and peridotitic mantle lithosphere.
Evolved, less dense, andesitic magmas rise into the mid-to-upper crust where they pool 三バカ大将を無料で見よ their new level of neutral buoyancy to form batholithic complexes.
Along with volcanic structures, porphyry and epithermal deposits may form at shallower levels above these batholithic complexes where exsolved magmatic fluids ascend, cool, and interact with near-surface upper crustal rocks.
Modified fromRichards 2003, 2005 ; sources: Hildreth andMoorbath 1988 ,Winter 2001Annen et al.
Post-subduction tectonic environments conducive to the formation of porphyry and epithermal deposits by remobilization of previously subduction-modified lithosphere modified from Richards, 2009.
Such magmas may remobilize Au as well as Cu±Mo left behind in residual sulfide phases by arc magmatism, leading to the potential formation of porphyry Cu±Au±Mo and alkalic-type epithermal Au deposits.
See text for discussion.
Schematic cross-section through a typical coupled arc batholith.
Also shown are the thermal structure, fluid flow pathways and characteristics during the main stage of hydrothermal activity, and overlapping hydrothermal alteration zones.
Propylitic alteration by circulating heated groundwaters can be assumed to affect all the supracrustal rocks in the field of view, with greatest intensity epidote, actinolite close to the intrusions, fading to background distally.
Modified from Richards 2005 ; sources: Sillitoe 1973, 2010Dilles 1987Shinohara and Hedenquist 1997Hedenquist et al.
Also shown are the ages of the various deposits and etallogenic provinces mentioned in the book.
Base metals include Cu, Pb, and Zn filled dotsand precious metals comprise Au, Ag, and Hg open circles.
The numbers next to individual points or ranges refer to average concentrations or ranges in a variety of different situations, and are all after Seward and Barnes 1997.
The length of each histogram bar is an estimate of the proportion of ore formed over a 50 million year interval relative to the global resource for that deposit type.
Periods of supercontinent amalgamation are shown as Pangea, Rodinia, and Nena, with decreasing levels of confidence further back in time.
The diagram is originally after Meyer 1988 and modified after Barley and Groves 1992.
Phanerozoic porphyry belts, porphyry deposits, and representative porphyry copper deposits summarized in Appendix 2 red labels.
Modified from Seedorff and others 2005, their Fig.
General setting of porphyry copper and associated deposit types modified from Sillitoe and Bonham, 1990.
Detailed descriptions are provided in the text modified after the models of Candela and Holland, 1984; 1986; Strong, 1988; Candela, 1992.
Location of explored Nb- and REE-carbonatite deposits BMWの駐車場ゲームオンライン無料プレイ今すぐ in the database and grade and tonnage models.
Volcanogenic massive sulfide deposit subtypes mentioned in situation 無料ゲームスペインのカジノルーレット opinion paper.
World map showing the distribution of volcanogenic massive sulfide deposit subtypes.
Footwall rocks may consist of a sheeted dyke complex and the associated volcanics are often pillowed and have a tholeiitic composition.
After Hutchinson and Searle 1971.
Associated volcanics may be intermediate or felsic in composition and a closer lateral link to chemical and epiclastic sediments is often apparent.
The lens of massive sulfide ore formed on the ocean floor, underlain by a stockwork zone of disseminated sulfides and intensely altered volcanic rock, is typical of VMS deposits in general after Large, 1992.
Both diagrams after Large 1992.
Global distribution of Mississippi Valley-Type lead-zinc deposits and districts.
Deposits are associated with broad redox boundaries and feature sodic alteration of source rocks and 火エンブレムフラッシュゲームオンライン alteration of host rocks.
A genetic link between high-sulfidation epithermal Au?
Cu and sub-volcanic porphyry type Cu?
Au 金鉱床 is also suggested after Hedenquist et al.
The diagram is relevant to both Chapters 2 and 3, and is modified after Skinner 1997.
Ficklin plot of the sum of the base metals Cd, Co, Cu, Ni, Pb, and Zn versus pH illustrating the variation of mine drainage chemistry as a function of the geologic characteristics type of specific mineral deposits.
Modified from Plumlee and Nash 1995and Plumlee 1999.

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金鉱脈の発見から金の採掘まで、こうやって金はできあがる. 2015/08/14. gold-vein 宝飾品や芸術品、また財産の一部として、長い歴史の中で人類に愛されて、珍重されてきた金。 21世紀となった現在でも未だ多くの人々を魅了し続けています。 ところで、金.


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1961: 作曲ってコード理論など言われるけど、結局、センスなんだよ [805596214] (53)
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ある特定の時代に特徴的に形成されていることが分か. ります。 では、どこに. 4. 4. 4 形成されるか? まず、世界中の金属. 鉱床の位置を概観して見ましょう。〔資料 18〕~〔資. 料 21〕は世界の銅鉱床、亜鉛鉱床、ニッケル鉱床及. び金鉱床の.


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明石の改修工廠早見表 | Simplified Chart for Akashi
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金鉱床と火山フロント: 鹿児島大学総合研究博物館 から
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菱刈の金鉱脈の先端は、標高80~120mにあって、金の平均含量が80ppm(普通は6ppm以下)、予想採鉱可能な金含量が120トンという高品位の金鉱脈で、佐渡金山(新潟)の金鉱床の総生産量77トンを上回るということで、大きな話題.


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湯沸かし勇者の復讐譚〜水をお湯にすることしか出来ない勇者だけど、全てを奪ったお前らを殺すにはこいつで十分だ〜 - 78 坑道の赤い石
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月, 火, 水, 木, 金, 土, 日. マジックザギャザリング MTG 土地 英語版 露天鉱床/Strip Mine ATQ-82B アンコモン【ランクA】【中古】, (3); 2018年11月 (9); LED照明器具 LEDダウンライト(MCシリーズ) Φ100 深枠タイプ 鏡面コーン遮光30° EL-D23/1(250WH).


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Stratiform arkose-hosted and shale-hosted copper Zambian copperbelt.
Data from the synthesis of ore deposits.
Data plotted and diagrams prepared by W.
Cu-Mo Cu -Au Mo -W Skarn Mineral deposits formed by replacement of limestone by ore and calc-silicateminerals, usually adjacent to a felsic or granitic intrusive body.
Hypothermal - Cu -Au Mesothermal - Cu-Pb-Zn-Ag-Au Epithermal - Au-Ag -Hg Mississippi Valley Named for the region where they were first described, these deposits formed within porous carbonate rocks limestone reefs or caves.
They are Pb-Zn deposits with low Ag values.
Syngenetic Volcanic Massive Sulphide VMS These deposits formed as massive over 60% sulphide lens-like accumulations on or near the sea floor in association with volcanic activity.
Pb-Zn-Ag Ba Magmatic- layered mafic intrusion During the crystallization of a magma, usually mafic or ultramafic, heavy, metal-rich liquids settle and accumulate at 金鉱床 sites, often at the base, within the intrusion.
PGM Platinum group metals Chromite Ni-Cu -PGM Placer Formed within sediments by the concentration of heavy resistant minerals Au diamond, cassiterite by stream or wave action.
Iceland, in the north Atlantic, is the tip of one part of this mountain range.
Volcanogenic massive sulfide VMS deposits described in the text are an example of mineral deposits that form on the sea floor.
Also shown are convergent plate boundaries where an oceanic plate is being subducted beneath a continental tectonic plate forming folded and faulted mountains orogen and volcanoes.
The subduction of oceanic tectonic plates is accompanied by strong earthquakes and the generation and movement of tmagma molten rock and hydrothermal fluids that form a variety of mineral deposits, including porphyry copper deposits and associated gold and silver veins and polymetallic replacement deposits and associated gold and silver veins and polymetallic replacement deposits described in this report.
Continental rift zones are areas where the crust is stretched extended forming linear 金鉱床 characterized by faults, volcanoes, sedimentary basins, and a variety of mineral deposit types including sediment-hosted sedex lead-sinc, sediment-hosted copper, and evaporite deposits.
See text for further discussion.
Modified from Kious and Tilling 1996.
Compositional fields of arc volcanic rocks, high-temperature volcanic fumaroles, magmatic-hydrothermal fluids, and geothermal fluids are shown, as discussed by Einaudi et al.
Simplified from Einaudi et al.
Schematic sections of end-member volcanotectonic settings and associated epithermal and related mineralization types.
Calc-alkaline volcanic arc with neutral to mildly extensional stress state showing relationships between high- and intermediate-sulfidation epithermal and porphyry deposits note that the complete spectrum need not be present everywhere.
Later, less acidic intermediate-sulfidation fluid gives rise to ntermediate-sulfidation mineralization, both djacent to and distal from the advanced argillic lithocap.
Where the intermediate-sulfidation fluid flows through the leached lithocap environment, it evolves to a high-sulfidation fluid Einaudi et al.
The high-sulfidation fluid may evolve back to intermediate-sulfidation stability during late stages, supported by paragenetic relationships and lateral transitions of high- to intermediate-sulfidation mineralogy.
See text for details.
Rift with bimodal volcanism and low-sulfidation deposits.
Henley and Ellis, 1983; Giggenbach, 1992; John, 2001.
Structure and processes beneath an oceanic island arc sources: Tatsumi and Eggins, 1995; Schmidt and Poli, 1998; Winter, 2001; Poli and Schmidt, 2002; Fumagalli and Poli, 2005.
Primary hydrous basaltic arc magmas are derived from partial melting of the metasomatized asthenospheric mantle wedge.
Mineral zones shown in the subducting 金鉱床 indicate lower limits of stability of hydrous phases in the basaltic oceanic crust and peridotitic mantle lithosphere.
Evolved, less dense, andesitic magmas rise into the mid-to-upper crust where they pool at their new level of neutral buoyancy to form batholithic complexes.
Along with volcanic structures, porphyry and epithermal deposits may form at shallower levels above these batholithic complexes where exsolved magmatic fluids ascend, cool, and interact with near-surface upper crustal rocks.
Modified fromRichards 2003, 2005 ; sources: Hildreth andMoorbath 1988 ,Winter 2001Annen et al.
Post-subduction tectonic environments conducive to the formation of porphyry and epithermal deposits by remobilization of previously subduction-modified lithosphere modified from Richards, 2009.
Such magmas may remobilize Au as well as Cu±Mo left behind in residual sulfide phases by arc magmatism, 金鉱床 to the potential formation of porphyry Cu±Au±Mo and alkalic-type epithermal Au deposits.
See text for discussion.
Schematic cross-section through a typical coupled arc batholith.
Also shown are the thermal structure, fluid flow pathways and characteristics during the main stage of hydrothermal activity, and overlapping hydrothermal alteration zones.
Propylitic alteration by circulating heated groundwaters can be assumed to affect all the click rocks in the field of view, with greatest intensity epidote, actinolite close to the intrusions, fading to background distally.
Modified from Richards 2005 ; sources: Sillitoe 1973, 2010Dilles ゲームgba4iosShinohara and Hedenquist 1997Hedenquist et al.
Also shown are the ages of the various deposits and etallogenic provinces mentioned in the book.
Base metals include Cu, Pb, and Zn filled dotsand precious metals comprise Au, Ag, and Hg open circles.
The length of each histogram bar is an estimate of the proportion of ore formed over a 50 金鉱床 year interval relative to the global resource for that deposit type.
Periods of supercontinent amalgamation are shown as Pangea, Rodinia, and Nena, with decreasing levels of confidence further back in time.
The diagram is originally after Meyer 1988 and modified after Barley and Groves 1992.
Phanerozoic porphyry belts, porphyry deposits, and representative porphyry copper deposits summarized in Appendix 2 red labels.
Modified from Seedorff and others 2005, their Fig.
General setting of porphyry copper and associated 金鉱床 types modified from Sillitoe and Bonham, 1990.
Detailed descriptions are provided in the text modified after the models of Candela and Holland, 1984; 1986; Strong, 1988; Candela, 1992.
Location of explored Nb- and REE-carbonatite deposits included in the database and grade and tonnage models.
Volcanogenic massive sulfide deposit subtypes mentioned in this paper.
World map showing the distribution of volcanogenic massive sulfide deposit subtypes.
Footwall rocks may consist of a sheeted dyke complex and the associated volcanics are often pillowed and have a tholeiitic composition.
After Hutchinson and Searle 1971.
Associated volcanics may be intermediate or felsic in composition and a closer lateral link to chemical and epiclastic sediments is often apparent.
The lens of massive sulfide ore formed on the ocean floor, underlain by a stockwork zone of disseminated 金鉱床 and intensely altered volcanic rock, is typical of VMS deposits in general after Large, 1992.
Both diagrams after Large 1992.
Global distribution of Mississippi Valley-Type lead-zinc deposits and districts.
Deposits are associated with broad redox boundaries and feature sodic alteration of source rocks and potassic alteration of host rocks.
A genetic link between high-sulfidation more info Au?
Cu and sub-volcanic porphyry type Cu?
Au deposits is also suggested after Hedenquist et al.
The diagram is relevant to both Chapters 2 and 3, and is modified after Skinner 1997.
Ficklin plot of the sum of the base metals Cd, Co, Cu, Ni, Pb, and Zn versus pH illustrating the variation of mine drainage chemistry as click at this page function of the geologic characteristics type of specific mineral deposits.
Modified from Plumlee and Nash 1995apologise, パソコン用の無料ゲームのダウンロード opinion Plumlee 1999.

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菱刈の金鉱脈の先端は、標高80~120mにあって、金の平均含量が80ppm(普通は6ppm以下)、予想採鉱可能な金含量が120トンという高品位の金鉱脈で、佐渡金山(新潟)の金鉱床の総生産量77トンを上回るということで、大きな話題.


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青ヶ島沖に金鉱床発見。 : 旅と暮らしの日々 by sato tetsuya
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金鉱床のでき方 常温では金は水に溶けないのだが、地下のマグマの熱と強い圧力のもと、300℃以上に熱せられた地中深くの熱水により、鉱物から溶かし出される。熱水は地表に向けて上昇しながら、圧力や温度の低下により沸騰し、また、.


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青ヶ島沖に金鉱床発見。 : 旅と暮らしの日々 by sato tetsuya
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ロシア、金鉱床開発に関する中国との合意書を承認 | 海外ビジネスニュースを毎日配信!− DIGIMA NEWS
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[ScienceNews2016]海底資源を「養殖」 人工チムニー開発(2016年9月2日配信)

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恐山周辺地域金鉱床賦存状況調査」によると、局部的に鉱石1トン当たり463g、最高で6500gという極めて高い含有率を示している金の鉱脈。


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青ヶ島沖に金鉱床発見。 : 旅と暮らしの日々 by sato tetsuya
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湯沸かし勇者の復讐譚〜水をお湯にすることしか出来ない勇者だけど、全てを奪ったお前らを殺すにはこいつで十分だ〜 - 78 坑道の赤い石
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2012年12月12日、今年の世相を表す「今年の漢字」に「金」が選ばれた。ロンドンオリッピックの. 一方、2012年10月9日、住友金属鉱山は、金を産出する菱刈鉱山(鹿児島県伊佐市)で新たな金鉱床を発見したと発表した。埋蔵量は約30トン、.


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山東省莱州付近の海域で超大型金鉱床を発見、資源量470トン超_中国網_日本語
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海底熱水鉱床の連続揚鉱に成功

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cinii上で見つけた「貫入岩に関係する鉱脈型金鉱床:そのタイプ・構造-マグマ活動的背景,そして造山期金鉱床との識別の難しさ」Intrusion-Related Vein Gold Deposits : Types, Tectono-Magmatic Settings and Difficulties of Distinction.


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ロシア、金鉱床開発に関する中国との合意書を承認 | 海外ビジネスニュースを毎日配信!− DIGIMA NEWS
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山東省莱州付近の海域で超大型金鉱床を発見、資源量470トン超_中国網_日本語
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