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Low-temperature mineralization domain associated with the parallel positions between geochemical steep zones and geophysical gradient zones

机译:与地球化学陡峭带和地球物理梯度带之间的平行位置相关的低温矿化区域

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摘要

The parallel strike of geochemical steep zones and geophysical gradient zones represent geochemical boundaries with tectonic hiding and almost no magmatism, but there existed great variation of lithosphere or crustal thickness. Tectonically, these areas were located in the foreland basins of carton margin. These geochemical boundaries wer usually associated with the low-temperature mineralization and petroleum generation.
机译:地球化学陡峭带和地球物理梯度带的平行走向代表了具有构造隐蔽性和几乎没有岩浆作用的地球化学边界,但岩石圈或地壳厚度存在很大的变化。从构造上讲,这些区域位于纸箱边缘的前陆盆地中。这些地球化学边界通常与低温矿化和石油产生有关。

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