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摘要:
Metallogenic specialization of sedimentary cover in Central Asia is determined by its tec-tonic setting that governs the hydrodynamic regime (exfiltrational or infiltrational) and as a consequence, the hydrogeochemical zonality (type of water and its gaseous and microcomponent composition). Hydro-dynamic conditions (distribution of recharge and discharge areas) determine the direction of stratal wa-ter flow and location of mineralization resulted from the change in geochemical, thermodynamic, litholog-ical, structural and other conditions. The exfiltrational regime suggests a dependence of the epigenetic mineralization upon the distribution and degree of preservation of hydrocarbon occurrences. Often, hy-drocarbon matter serves as a reducing barrier and ore-concentrating factor during the formation of polymineral concentrations related to stratal oxidation zone. The supergene epigenetic ore-forming pro-cesses are induced by the interaction between the Earth ' s sedimentary cover and hydrosphere. Sedimen-tary rocks themselves commonly serve as a source of ore materials. The ore deposition zones on geochemi-cal barriers and ore material source are often located significantly apart from each other. The trend of these processes is determined by the position of ore-bearing depressions in large tectonic blocks.
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篇名 Central Asia––A Global Model for the Formation of Epigenetic Deposits in a Platform Sedimentary Cover
来源期刊 地球科学学刊(英文版) 学科
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年,卷(期) 2022,(2) 所属期刊栏目 Special Issue on Sandstone-Type Uranium Mineralization and Its Metallogenic Background
研究方向 页码范围 278-288
页数 11页 分类号
字数 语种 英文
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地球科学学刊(英文版)
双月刊
1674-487X
42-1788/P
大16开
武汉市洪山区鲁磨路388号
38-354
1990
eng
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