内蒙古二连盆地白音查干凹陷下白垩统腾格尔组热水沉积过程中矿物沉淀顺序及其控制因素*
钟大康1,2, 苏琛1,2, 杨喆1,2, 贾晓兰1,2

Precipitation sequence of hydrothermal minerals and their controlling factors during the sedimentation: A case study of the Lower Cretaceous Tenggeer Formation in Baiyinchagan sag of Erlian Basin,Inner Mongolia
Zhong Da-Kang1,2, Su Chen1,2, Yang Zhe1,2, Jia Xiao-Lan1,2
内蒙古二连盆地白音查干凹陷下白垩统腾格尔组纹层和团块中矿物的QemScan图像(25 μm扫描精度) 自下而上由铝硅酸盐纹层向碳酸盐纹层顺序过渡(6~19 mm);铝硅酸盐内部(0~6 mm;19~27 mm)由沸石—钠长石—钾长石向钠长石—钾长石的顺序过渡;凝絮团块内由铝硅酸盐向碳酸盐顺序过渡。锡3-69井,1772.2 m,柱塞样薄片