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- W2361518888 abstract "The copper, gold and sulfide ore deposits of Tongguanshan, Dongguashan and Xinqiao etc. in China occurred at or near the surface of unconformity or disconformity between sandstone, quartz sandstone of Wutong group, Upper Devonian and carbonate rocks of Huanglong group, Middle and Upper Carboniferous. Researches show that there are two geological events responsible for forming the ore deposits with the same or similar genesis in that district: (1) the district possesses specific lithologic characteristics as well as a specific suite of strata; (2)the suite of strata was intruded by the related magma which carried along the associated thermal energy and the ore|forming materials.The thermal energy drived the ore|forming fluids and caused them to circulate around the intrusive bodies.When the fluid flowed from the pyrite|bearing sandstone to the surface of disconformity,the ore|forming process of fluid flow|mineral dissolution|material transportation|ore precipitation took place.The authors put forward a set of partial differential equations to model the ore|formig process of copper,gold and sulfides in the district,and carries out the computer simulation and dynamical analysis for the processes." @default.
- W2361518888 created "2016-06-24" @default.
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- W2361518888 date "2001-01-01" @default.
- W2361518888 modified "2023-09-25" @default.
- W2361518888 title "COUPLED SYSTEM OF FLOW-REACTION- TRANSPORTATION OF ORE-FORMING FLUID AND METALOGENESIS" @default.
- W2361518888 hasPublicationYear "2001" @default.
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