热水沉积岩岩石学特征:以内蒙古二连盆地白音查干凹陷下白垩统腾格尔组为例*
钟大康1,2, 杨喆1,2, 孙海涛1,2, 张硕3

Petrological characteristics of hydrothermal-sedimentary rocks:A case study of the Lower Cretaceous Tengger Formation in the Baiyinchagan Sag of Erlian Basin, Inner Mongolia
Zhong Da-Kang1,2, Yang Zhe1,2, Sun Hai-Tao1,2, Zhang Shuo3
内蒙古二连盆地白音查干凹陷热水沉积岩泥晶结构和团块结构显微特征 A—含铁白云石泥晶结构,锡36井,2429.2,m,正交偏光;B—铁白云石—钠沸石组合泥晶结构,锡26井,1824.3,m,正交偏光;C—泥晶白云石—钠沸石混杂基质,锡26井,1832,m,正交偏光;D—粉细晶白云石团块,锡26井,1812.73,m,正交偏光;E—钠沸石团块, 锡26井,1816.33,m,正交偏光;F—方沸石团块,边缘被泥晶白云石胶结,锡36井,2436.94,m,正交偏光