hydrothermal alteration的意思
hydrothermal alteration中文翻譯:
[地質]熱液蝕變;水熱蝕變
hydrothermal───adj.[地質]熱液的;熱水的
alteration───n.修改,改變;變更
alteration skyrim───部分
chloritic alteration───綠泥石蝕變
hydrothermal vent───深海熱泉;深海熱液噴口
hypogene alteration───深成蝕變
alteration movie───涂改片
alteration nearby───附近蝕變
alteration okc───變更okc
In Nanla area, the vegetation colour anomaly on remote sensing image is a reflection of the hydrothermal alteration, which can be regarded as an indirect indication in ore prospecting.───南臘地區遙感影像圖上植被的褪色現象,認為是熱蝕變的反映,可以作為找礦的間接標志。
Taoyuan molybdenum ore belongs to mesothermal hydrothermal vein deposit. Alteration of country rock has linear feature.───桃園鉬礦床屬中溫熱液脈型礦床,圍巖蝕變具線型對稱特征。
Hydrothermal alteration is closely associated with gold mineralization, but different types play different roles in gold mineralization.───熱液蝕變與金礦化關系密切,但不同的蝕變對金礦化作用不同。
Quartz, serpentine and chlorite are minerals commonly associated with hydrothermal alteration.───石英,蛇紋石及綠泥石均為常見的與熱液蝕變作用伴生的礦物。
Hydrothermal Alteration and Ore-forming Fluids Evolution of the Jingxi-Yelmend Gold Deposit, Xinjiang, China───伊犁京希-伊爾曼德金礦床的熱液蝕變及成礦流體演化特征
Gold Mineralization Styles of Jingxi-Yelmend Deposit: Evidence from Hydrothermal Alteration and Fluid Inclusion Data───新疆京希-伊爾曼德金礦床礦化類型:熱液蝕變及流體包裹體證據
Geological- geochemical Features of Ore- near Hydrothermal Alteration Rocks in Pangushan Tungsten Deposit───盤古山鎢礦床近礦熱液蝕變巖石的地質地球化學
As well as the crushing effects described above, many of the rocks in the thrust zone suffered hydrothermal alteration.
Arsenian pyrite is the most important Au-bearing mineral, and silicification with quartz veins is the well-marked hydrothermal alteration.
These hills result from hydrothermal alteration of the granites which are characteristic of the area.
Illite jade, in vein, was discovered in some copper mine, located in Daye county, HubeiProvince, and is a rind hydrothermal alteration rock from anorthosite.
The ultrabasic rocks have been extensively affected by several phases of hydrothermal alteration.
Gold bodys are metasomatic vains, and was generated by diorite and surrounding rock which suffered multi-stage breccia, silicification and sericite hydrothermal alteration.
Hydrothermal alteration and mineralisation continued for up to 30 Ma after the emplacement of the intrusions at about 400 Ma.
It is common for almost all of large_and medium_size hydrothermal deposits to develop widespread hydrothermal alteration, accompanied by inspissation of ore_forming fluids.
It is cinnabar and dickite, kaolinite petrochemical and hydrothermal alteration of the product of mercury.
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