塔里木盆地东北缘兴地断裂以北地区下寒武统富有机质泥页岩沉积环境与发育机制*
胡宗全1,2,3, 高志前4, 刘旺威5, 卫端4

Depositional environments and formational mechanisms of the Lower Cambrian organic-rich mud/shales, north of Xingdi Fault, northeastern Tarim Basin
HU Zongquan1,2,3, GAO Zhiqian4, LIU Wangwei5, WEI Duan4
依据岩石矿物成分的细粒沉积岩命名原则 (修改自 Lazar et al ., 2015 )