上一条： Depositional facies and diagenesis of the Lianglitage Formation in northwestern Tazhong Uplift, Tarim Basin, China: implications for the genesis of ultra-deep limestone reservoir

下一条： 塔中地区晚奥陶世碳酸盐台地边缘与台地内部的沉积差异——定性和定量的碳酸盐岩微相综合分析