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鄂尔多斯盆地南缘奥陶系顶部碳酸盐岩风化壳特征及其成因机制*
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熊加贝1,2,3, 何登发2,3, 成祥2,3, 罗瑀峰1 |
Characteristics and genetic mechanism of weathering crust on carbonate rocks on the top of the Ordovician in southern margin of Ordos Basin
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XIONG Jiabei 1,2,3, HE Dengfa 2,3, CHENG Xiang 2,3, LUO Yufeng 1
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鄂尔多斯盆地南缘洛1井本溪组—马家沟组岩心照片 a—含泥白云岩,见长条状与椭圆状角砾,马家沟组,2771.9 m;b—灰质白云岩,见垂直裂缝,马家沟组,2773.95 m;c—碳质泥岩,见黄铁矿斑块,本溪组,2764.0 m;d—煤岩,见黄铁矿斑块,本溪组,2764.36 m;e—铝土质泥岩,见植物化石,马家沟组,2766.8 m; f—泥岩,见植物叶片,马家沟组,2767.5 m |
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