Tectonic-lithofacies paleogeography, large-scale source- reservoir distribution and exploration zones of Cambrian subsalt formation, Tarim Basin, NW China |
WEI Guoqi,ZHU Yongjin,ZHENG Jianfeng,YU Guang,NI Xinfeng,YAN Lei,TIAN Lei,HUANG Lili |
Fig. 1. Schematic tectonic provinces in the Tarim Basin (a), north-south structural-stratigraphic section (b), and generalized stratigraphic column (c). ① Member 2 of the Upper Xiaoerbulak Fm.; ② Member 1 of the Upper Xiaoerbulak Fm.; ③ Member 3 of the Lower Xiaoerbulak Fm.; ④ Member 2 of the Lower Xiaoerbulak Fm.; ⑤ Member 1 of the Lower Xiaoerbulak Fm. AnZ—Pre-Sinian;Nh—Nanhua;Z—Sinian;—C1+2—Middle and Lower Cambrian;—C3—Upper Cambrian;O1—Lower Ordovician;O2+3—Middle-Upper Ordovician;S—Silurian;D—Devonian;C—Carboniferous;P—Permian;T—Triassic;K—Cretaceous;E—Paleogene;N1j—Neogene Jidike Formation;N1k—Neogene Kangcun Formation;N2k—Neogene Kucha Formation. |