During the field season of 1982 in Northern Junggar Basin, surface collecting by the field party of IVPP at the outcrops of Halamagai Formation provided 7 isolated cheek teeth of rodents associated with some macromamm...During the field season of 1982 in Northern Junggar Basin, surface collecting by the field party of IVPP at the outcrops of Halamagai Formation provided 7 isolated cheek teeth of rodents associated with some macromammals typical of middle Miocene age: Platybelodon, Stephanocemas thomsoni, Lagomeryx sp., etc.It is the first time that the Miocene rodents are discovered in this region. They belong to 3 genera, 4 species:Sinomylagaulus halamagaiensis gen. et sp. nov.Atlantoxerus junggarensis sp. nov.A. giganteus sp. nov.Amblycastor tungurensis Stirton, 1934Many thanks are due to Drs. V. Fahlbusch, N. Schmidt-Kittler, P. Mein and N. S. Shevyreva for their sending me the comparative materials, reprints and profitable discussion. The colleagues of IVPP field party put in a lot of hard work to collect this material. Mr. Shen Wenlong made the textfigures. To all these persons the author wants to express her heartfelt gratitudes.All the specimens herein described are stored in the collections of IVPP.展开更多
Geological mapping,interpreted cross sections,structural analyses and residual thickness maps were used to characterize the evolution of stress setting,structure and stratigraphic distribution of the Chepaizi Uplift,w...Geological mapping,interpreted cross sections,structural analyses and residual thickness maps were used to characterize the evolution of stress setting,structure and stratigraphic distribution of the Chepaizi Uplift,which is a NW-SE trending structure located in the Western Junggar Basin.The NS-trending faults show an important transpressional phase during the Late Permian,as demonstrated by tectonic stress field and stratigraphic thickness variations.A major compressional thrusting and strike-slip phase during the Late Jurassic created a series of NW-SE faults that originated by the large-scale uplift event in the Northern Tianshan.Faults were reactivated as thrust and dextral strike-slip faults.In addition,the angular unconformity observed between Jurassic and Cretaceous provide evidence of this tectonic event.Lots of normal faults indicate that the area records southward tilting and regional derived extensional stress that took place during the Neogene.Before that,thick Early Cenozoic strata are widely deposited.The balanced cross-section highlights the evolution of stress setting and stratigraphic distribution of the Chepaizi Uplift.展开更多
文摘During the field season of 1982 in Northern Junggar Basin, surface collecting by the field party of IVPP at the outcrops of Halamagai Formation provided 7 isolated cheek teeth of rodents associated with some macromammals typical of middle Miocene age: Platybelodon, Stephanocemas thomsoni, Lagomeryx sp., etc.It is the first time that the Miocene rodents are discovered in this region. They belong to 3 genera, 4 species:Sinomylagaulus halamagaiensis gen. et sp. nov.Atlantoxerus junggarensis sp. nov.A. giganteus sp. nov.Amblycastor tungurensis Stirton, 1934Many thanks are due to Drs. V. Fahlbusch, N. Schmidt-Kittler, P. Mein and N. S. Shevyreva for their sending me the comparative materials, reprints and profitable discussion. The colleagues of IVPP field party put in a lot of hard work to collect this material. Mr. Shen Wenlong made the textfigures. To all these persons the author wants to express her heartfelt gratitudes.All the specimens herein described are stored in the collections of IVPP.
基金financially supported by the Natural Sciences Foundation of China(Chen S.,grant number 41502208)Science Foundation of China University of Petroleum(Chen S.,grant number 2462017BJB01)CNPC Innovation Foundation(Chen S.,grant number 2017D-5007-0103)
文摘Geological mapping,interpreted cross sections,structural analyses and residual thickness maps were used to characterize the evolution of stress setting,structure and stratigraphic distribution of the Chepaizi Uplift,which is a NW-SE trending structure located in the Western Junggar Basin.The NS-trending faults show an important transpressional phase during the Late Permian,as demonstrated by tectonic stress field and stratigraphic thickness variations.A major compressional thrusting and strike-slip phase during the Late Jurassic created a series of NW-SE faults that originated by the large-scale uplift event in the Northern Tianshan.Faults were reactivated as thrust and dextral strike-slip faults.In addition,the angular unconformity observed between Jurassic and Cretaceous provide evidence of this tectonic event.Lots of normal faults indicate that the area records southward tilting and regional derived extensional stress that took place during the Neogene.Before that,thick Early Cenozoic strata are widely deposited.The balanced cross-section highlights the evolution of stress setting and stratigraphic distribution of the Chepaizi Uplift.
