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*
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
XIONG Jiabei1,2,3, HE Dengfa2,3, CHENG Xiang2,3, LUO Yufeng1
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