0 INTRODUTION The Kuqa Depression,situated along the northern margin of the Tarim Basin,holds substantial geological significance due to its intricate sedimentary burial history,tectonic history,and the evolution of h...0 INTRODUTION The Kuqa Depression,situated along the northern margin of the Tarim Basin,holds substantial geological significance due to its intricate sedimentary burial history,tectonic history,and the evolution of hydrocarbon source rocks(Jiang et al.,2024;Zhang et al.,2023;Huang et al.,2019;Yang et al.,2017;Jia et al.,2003;Hendrix,2000).展开更多
The Altai-Sayan region,an active intracontinental mountain belt characterized by high relief,has undergone multiple phases of intense mountain building and denudation throughout the Mesozoic and Cenozoic.As this mount...The Altai-Sayan region,an active intracontinental mountain belt characterized by high relief,has undergone multiple phases of intense mountain building and denudation throughout the Mesozoic and Cenozoic.As this mountain belt with remarkable topography is distant from any active plate margins,its mountain growth pattern and tectonic reactivation mechanism are of great significance to the study of intracontinental orogeny.展开更多
基金supported by the National Key Research and Development Project(No.2019YFA0708601)the National Natural Science Foundation of China(No.4231101056)the Chinese Academy of Geological Sciences Basic Research Fund(No.JKYZD202402)。
文摘0 INTRODUTION The Kuqa Depression,situated along the northern margin of the Tarim Basin,holds substantial geological significance due to its intricate sedimentary burial history,tectonic history,and the evolution of hydrocarbon source rocks(Jiang et al.,2024;Zhang et al.,2023;Huang et al.,2019;Yang et al.,2017;Jia et al.,2003;Hendrix,2000).
基金financially supported by the China Geological Survey(No.DD20230213)the National Key Research and Development Project(No.2019YFA0708601)Shanxi Province Natural Science Foundation(No.2020JM-310)。
文摘The Altai-Sayan region,an active intracontinental mountain belt characterized by high relief,has undergone multiple phases of intense mountain building and denudation throughout the Mesozoic and Cenozoic.As this mountain belt with remarkable topography is distant from any active plate margins,its mountain growth pattern and tectonic reactivation mechanism are of great significance to the study of intracontinental orogeny.
