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<sup>*</sup>

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 Zongquan^1,^2,³, GAO Zhiqian⁴, LIU Wangwei⁵, WEI Duan⁴

塔里木盆地东北缘下寒武统各类岩石U_EF-Mo_EF交汇图(图版引自 Tribovillard et al ., 2012 )