Zobrazeno 1 - 10
of 60
pro vyhledávání: '"Xianzhi Pei"'
High-pressure and ultrahigh-pressure minerals tend to be preserved in mafic and ultramafic metamorphic rocks, such as eclogites and garnet amphibolites, rather than felsic rocks. Generally, the garnet amphibolites preserve particular porphyroblastic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3f16114f1ca4d3c9f68998f436641811
https://doi.org/10.5194/egusphere-egu23-4041
https://doi.org/10.5194/egusphere-egu23-4041
Autor:
Meng Wang, Xianzhi Pei, Zuochen Li, Ruibao Li, Lei Pei, Youxin Chen, Chengjun Liu, Shaowei Zhao
The West Qinling Orogen (WQO), which is bounded by the Qilian Orogenic Belt, Qaidam Block and the Songpan-Ganzi Block, is the western extension of the Qinling Orogenic Belt, and experienced complex tectonic evolution processes, involving the opening,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ae8535cec3dc02a8c923b4124f36bc28
https://doi.org/10.5194/egusphere-egu23-2521
https://doi.org/10.5194/egusphere-egu23-2521
Autor:
Ruibao Li, Xianzhi Pei, Zuochen Li, Lei Pei, Guochao Chen, Zhanqing Liu, Youxin Chen, Chengjun Liu, Meng Wang
The East Kunlun Orogen on the northern margin of the Tethyan orogenic system records a history of Gondwana dispersal and Laurasian accretion. Based on a synthesis of sedimentary, structural, lithological, geochemical, and geochronological data from t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7f13ee5203e08ad04c67e5344d6e8ba0
https://doi.org/10.5194/egusphere-egu23-17000
https://doi.org/10.5194/egusphere-egu23-17000
During Carboniferous time, tremendous juvenile arc crust was formed in the southern Central Asian Orogenic Belt (CAOB), although its origin remains unclear. Our work presented zircon U-Pb-Hf and whole-rock geochemical and Sr-Nd isotopic data for a su
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e37706c0818c9aa50f1dc5b4fa2dfb4f
https://doi.org/10.5194/egusphere-egu23-66
https://doi.org/10.5194/egusphere-egu23-66
Autor:
Bo Zhang, Rong Ren, Meng Wang, Zuochen Li, Maohui Ge, Jinjiang Zhang, Youxin Chen, Xianzhi Pei
Publikováno v:
Gondwana Research. 105:185-200
Combining detrital zircon (DZ) U-Pb age and Lu-Hf isotope data is important in revealing the tectonic evolution of ancient orogens. Here, we conducted DZ U-Pb and Lu-Hf isotope research on 7 modern river sand samples collected from the northern Chine
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::52271359cae5540c626687db97160241
https://doi.org/10.1016/j.gr.2021.09.006
https://doi.org/10.1016/j.gr.2021.09.006
Autor:
Zuochen Li, Xianzhi Pei, Lei Pei, Chengjun Liu, Lili Xu, Ruibao Li, Hao Lin, Mao Wang, Shang Ji, Li Qin, Yajie Yang, Meng Wang, Shaowei Zhao, Youxin Chen
Publikováno v:
Minerals
Volume 13
Issue 2
Pages: 290
Volume 13
Issue 2
Pages: 290
The rhyolites which are widely exposed to the northern margin of the East Kunlun orogenic belt were chosen as a research object to discern the post-orogenic tectonic evolution of the East Kunlun orogenic belt and reconstruct the post-collision orogen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::72f3ec918f26326543d34bcd9940e30f
Autor:
Yigui Han, Orsoo Enkh-Orshikh, Qian Zhao, Donghai Zhang, Hai Zhou, Liu Qian, Xianzhi Pei, Guochun Zhao
Publikováno v:
Gondwana Research. 97:34-50
Tremendous granites were produced during the late-stage evolution of the Central Asian Orogenic Belt and important to understanding the tectonic processes from subduction to collision. Here, we present zircon U-Pb-Hf, and whole-rock geochemical, and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::60503b8baa305109aac96c0ff4164ded
https://doi.org/10.1016/j.gr.2021.05.005
https://doi.org/10.1016/j.gr.2021.05.005
Publikováno v:
Minerals; Volume 13; Issue 5; Pages: 651
Late Paleozoic–early Mesozoic intrusive rocks are distributed widely along the northern margin of the Qaidam Basin in the northern Tibetan Plateau. To constrain the tectonic evolution, we carried out petrological, chronological, and geochemical stu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1a1d28e7784520d178925b16112bf733
https://doi.org/10.3390/min13050651
https://doi.org/10.3390/min13050651
Autor:
Shang Ji, Zuochen Li, Xianzhi Pei, Lei Pei, Ruibao Li, Chengjun Liu, Youxin Chen, Hao Lin, Mao Wang
Publikováno v:
Minerals; Volume 13; Issue 4; Pages: 557
The North China Block and the South China Block collided in the Middle Triassic, but there is still a lack of consensus regarding the end of collisional orogeny and the closure time of the Paleo-Tethys. In this paper, we report zircon U–Pb ages and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::164a0d1f740c2f4247d79a489ba2bb1f
https://doi.org/10.3390/min13040557
https://doi.org/10.3390/min13040557
Publikováno v:
Minerals; Volume 13; Issue 4; Pages: 532
The transition from the Proto- to the Paleo-Tethys is still a controversial issue. This study reports a new petrology, zircon U–Pb geochronology, and whole-rock geochemistry of volcanic rocks from the Maoniushan Formation in the Nankeke area, north
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::97f0a4fb18d6a1683f21a8342c35a3b0
https://doi.org/10.3390/min13040532
https://doi.org/10.3390/min13040532