Earth Science Frontiers ›› 2023, Vol. 30 ›› Issue (4): 19-42.DOI: 10.13745/j.esf.sf.2022.10.18
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HE Bizhu1,2(), JIAO Cunli3, LIU Ruohan1,4, CAO Zicheng5, CAI Zhihui1, LAN Mingjie5, YUN Xiaorui1,3, ZHU Ding5, JIANG Zhongzheng5, YANG Yujie5, LI Zhenyu1,6
Received:
2022-08-20
Revised:
2022-09-29
Online:
2023-07-25
Published:
2023-07-07
CLC Number:
HE Bizhu, JIAO Cunli, LIU Ruohan, CAO Zicheng, CAI Zhihui, LAN Mingjie, YUN Xiaorui, ZHU Ding, JIANG Zhongzheng, YANG Yujie, LI Zhenyu. The paleotectonic and paleogeography reconstructions of the Tarim Basin in the Neoproterozoic and prediction of favorable deep source rock areas[J]. Earth Science Frontiers, 2023, 30(4): 19-42.
Fig.2 Sedimentary features of Cryogenian rocks(A-E) and structural architecture features of unconformities between the Cryogenian and Ediacaran (A,D-E), the Youermeinak section, Aksu area
Fig.4 Composite stratigraphic column of the Neoproterozoic northwestern margin and western and central parts of the Tarim Basin. Modified after [12,19,28,43].
Fig.6 West-east sedimentary succession from the Neoproterozoic to the Lower Cambrian along transect AA' (transect location see Fig.1). Youermeinake/Heishan sections modified after [10,19,34]; LT1 section modified after [32].
Fig.7 Structural architecture features of unconformities between the Cryogenian and the Ediacaran and between the Ediacaran and Cambrian (a-b), and wave-impedance profile (c) at the east part of the Tarim Basin (profile locations see Fig.9)
Fig.8 Structrual architecture features of unconformities between the Cryogenian and Ediacaran and between the Ediacaran and Cambrian(a-c), and the wave-impedance profile(d) in the Tarim Basin (profiles see in Fig.9)
Fig.9 Structural architecture features of unconformities and seismic stratigraphic attributes in the Neoproterzoic Tarim Basin. Fault systems modified after [12].
Fig.11 Tectono-sedimentary cycles and evolution of Neoproterozoic rift depressions, Tarim Basin (The Yingjisu faulted-depression is taken as an example (Profile i-iii indicate the three cycles in the Neoproterozoic, profile iv indicates the present features), and the relevant references of magmatic events are also marked.)
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