Zobrazeno 1 - 10
of 44
pro vyhledávání: '"Zhaogang SHAO"'
Autor:
Ye Wang, Xuanhua Chen, Chengguang He, Yongjun Xiao, Zhaogang Shao, Jian’en Han, Bing Li, Yiping Zhang, Weicui Ding, Shenglin Xu, Lele Han
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
The Yumu Shan is located at the northern margin of the Tibetan Plateau in northwest China. It is characterized by the development of several northeastward-protruding arcuate geomorphic bulge belts on its north slope. These bulge belts are distributed
Externí odkaz:
https://doaj.org/article/b75606fafbd54d0db090a0460b548972
Publikováno v:
Geological Journal. 58:1760-1775
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::336f848e60d27ccf76f572dcb6a0d767
https://doi.org/10.1002/gj.4692
https://doi.org/10.1002/gj.4692
Publikováno v:
Acta Geologica Sinica - English Edition. 97:13-34
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c9f6294ec74588c93c51bc4a171b2e8a
https://doi.org/10.1111/1755-6724.15007
https://doi.org/10.1111/1755-6724.15007
Autor:
Jie Li, Chen Wu, Xuanhua Chen, An Yin, Andrew V. Zuza, Peter J. Haproff, Yanfei Chen, Luojuan Wang, Zhaogang Shao
Publikováno v:
Geosphere. 19:100-138
High-pressure metamorphic rocks occur as distinct belts along subduction zones and collisional orogens or as isolated blocks within orogens or mélanges and represent continental materials that were subducted to deep depths and subsequently exhumed t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d6e23f38053bea8faea4da549c98ddc3
https://doi.org/10.1130/ges02548.1
https://doi.org/10.1130/ges02548.1
Publikováno v:
International Journal of Earth Sciences. 111:2369-2390
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5e6b688c53db27b9792a6f225514a43e
https://doi.org/10.1007/s00531-022-02233-x
https://doi.org/10.1007/s00531-022-02233-x
Publikováno v:
GSA Bulletin. 135:819-851
The Beishan orogen is part of the Neo-proterozoic to early Mesozoic Central Asian Orogenic System in central Asia that exposes ophiolitic complexes, passive-margin strata, arc assemblages, and Precambrian basement rocks. To better constrain the tecto
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3aabf2f691d3e026054fc3f24df2cc46
https://doi.org/10.1130/b36451.1
https://doi.org/10.1130/b36451.1
Autor:
Zhaogang Shao, Xuanhua Chen, Yuelei Yuan, Shengkai Qin, Yanfei Chen, Zuolin Tian, Zeming Zhang, Xin Dong
Publikováno v:
Acta Geologica Sinica - English Edition. 96:891-903
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::70e693d5babd29e1a5c6f12881e480dd
https://doi.org/10.1111/1755-6724.14796
https://doi.org/10.1111/1755-6724.14796
Autor:
Lele HAN, Weicui DING, Xuanhua CHEN, Zhaogang SHAO, Da ZHANG, Yongjun XIAO, Chengguang HE, Zengzhen WANG, Bing LI, Yiping ZHANG, Shenglin XU, Ye WANG
Publikováno v:
Acta Geologica Sinica - English Edition.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bb398a473f21bca362c6e960a7b98eed
https://doi.org/10.1111/1755-6724.15060
https://doi.org/10.1111/1755-6724.15060
Publikováno v:
Geological Journal. 57:3706-3720
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b20d8035e38c9d45e7b49e575a1eca62
https://doi.org/10.1002/gj.4497
https://doi.org/10.1002/gj.4497
Cenozoic deformation in the eastern domain of the North Qaidam thrust belt, northern Tibetan Plateau
Autor:
Bing Li, Yongchao Wang, Andrew V. Zuza, Xuanhua Chen, Zhaogang Shao, Zeng-Zhen Wang, Yujun Sun, Chen Wu
Publikováno v:
GSA Bulletin. 135:331-350
The present topography of the northern Tibetan Plateau is characterized by the northwest-trending Eastern Kunlun Range, Qaidam Basin, and Qilian Shan, which figure importantly into the evolution and mechanism of Tibetan plateau development during Cen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::64fcc0dfd5fc34c50711a3fc89e6338f
https://doi.org/10.1130/b36215.1
https://doi.org/10.1130/b36215.1