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塔里木盆地阿克苏沙井子地区康克林组为晚石炭世－早二叠世的一套碳酸盐与陆源碎屑混合沉积物，其岩性自下而上可分为：第一岩性段主要为石英砂岩、粉砂岩夹砾岩和砾屑灰岩；第二岩性段主要为灰岩与细砂岩或粉砂岩互层；第三岩性段主要为生屑灰岩、核形石灰岩夹砂屑灰岩。根据混合沉积物中碳酸盐和陆源碎屑的相对含量及组构特点可将其划分为八种形式：①碎屑岩夹灰岩；②碎屑岩与灰岩互层；③灰岩夹碎屑岩；④陆源碎屑散布于碳酸盐基质之中；⑤碳酸盐作为碎屑岩的填隙物；⑥碳酸盐颗粒散布于陆源碎屑之中；⑦陆源碎屑砾石与碳酸盐颗粒混合沉积；⑧陆源碎屑砾石和碳酸盐颗粒散布于碳酸盐基质之中。通过对混合沉积物形成机制的分析认为，混合物主要形成于潮坪至台地环境，海平面的变化严格控制着混合物的类型，碳酸盐沉积与海平面上升密切相关。
The Conklin Formation in the Aksu Shajingzi area, Tarim Basin, is a set of carbonate and terrigenous clastic sediments mixed in the Late Carboniferous-Early Permian. Its lithology can be classified from bottom to top: the first lithology is mainly quartz Sandstone, siltstone conglomerate and gravelly limestone; the second lithology is mainly interbedded limestone and fine sandstone or siltstone; the third lithology is mainly composed of bioclastic limestone, karyolite limestone, rock. According to the relative content of carbonate and terrigenous debris in the mixed sediments and their structural features, they can be divided into eight forms: clastic limestone, clastic rock and limestone interbed, limestone clamped Clastic rocks; ④ terrestrial debris dispersed in the carbonate matrix; ⑤ carbonate as clastic rock fillings; ⑥ carbonate particles scattered in terrestrial debris; ⑦ terrigenous clastic gravel and carbon Acid salt particles mixed deposition; ⑧ terrestrial debris gravel and carbonate particles dispersed in the carbonate matrix. Based on the analysis of the formation mechanism of mixed sediments, the mixture mainly formed in the tidal flat to the mesa environment. The change of sea level strictly controlled the type of mixture, and the carbonate deposition was closely related to the sea level rise.