|
二叠纪贵州遵义次级裂谷盆地结构及其对锰矿的控制作用*
|
刘志臣1,2, 周琦3, 颜佳新1, 汪洋2, 陈登1,2, 钟月丽2, 秦先进2 |
Structure of Zunyi rift basin in Guizhou Province during the Permian and its controlling on manganese deposits
|
Liu Zhi-Chen 1,2, Zhou Qi 3, Yan Jia-Xin 1, Wang Yang 2, Chen Deng 1,2, Zhong Yue-Li 2, Qin Xian-Jin 2
|
|
贵州遵义锰矿成矿模式 1—同沉积断层;2—锰矿层;3—凝灰岩;4—灰岩;5—硅质灰岩; 6—生物碎屑灰岩;7—硅化岩; 8—燧石条带灰岩;9—Ⅲ级断陷期富硅流体运移方向;10—Ⅳ级断陷期富锰流体运移方向 |
|
|
|
|
|