Zobrazeno 1 - 10
of 27
pro vyhledávání: '"Chongjin Zhao"'
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
The Songpan−Aba region is located on the northeastern edge of the Tibetan Plateau. Tectonically, the area is surrounded by the West Qinling orogenic belt in the north, the Longmenshan orogenic belt in the southeast, and the East Kunlun and Sanjiang
Externí odkaz:
https://doaj.org/article/eb4b4e7878fe4237b42ab1a46c54d1a8
Publikováno v:
Pure and Applied Geophysics. 180:23-39
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b5f3c34d8cbba4b420ece4f7aef8617d
https://doi.org/10.1007/s00024-022-03195-6
https://doi.org/10.1007/s00024-022-03195-6
Publikováno v:
GEOPHYSICS. 87:E307-E317
Except for producing smoothing models, magnetotelluric inversion also requires focused inversion, which can image sharp boundaries and clear interfaces of electrical structures. The proposed minimum support (MS) and minimum gradient support (MGS) hav
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d1229b3bb9c17e01cca836733fb795f1
https://doi.org/10.1190/geo2020-0485.1
https://doi.org/10.1190/geo2020-0485.1
Publikováno v:
GEOPHYSICS. 87:G97-G101
Normalized source strength (NSS) is often used to interpret remanence data owing to its low sensitivity to the direction of magnetization. However, calculations of NSS are unstable at low latitudes. Therefore, we have developed a new parameter called
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f80472836fe0d919481d42e377a78802
https://doi.org/10.1190/geo2021-0154.1
https://doi.org/10.1190/geo2021-0154.1
Publikováno v:
IEEE Transactions on Geoscience and Remote Sensing. 60:1-7
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b5565209169ef001d52cad9c624ac449
https://doi.org/10.1109/tgrs.2021.3138790
https://doi.org/10.1109/tgrs.2021.3138790
Autor:
Xi Xu, Hanlin Chen, Andrew V. Zuza, An Yin, Peng Yu, Xiubin Lin, Chongjin Zhao, Juncheng Luo, Shufeng Yang, Baodi Wang
Publikováno v:
Geology.
Deformation-resistant cratons comprise >60% of the continental landmass on Earth. Because they were formed mostly in the Archean to Mesoproterozoic, it remains unclear if cratonization was a process unique to early Earth. We address this question by
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7e128b180ef1704c76b16d95a8bb7299
https://doi.org/10.1130/g50615.1
https://doi.org/10.1130/g50615.1
Publikováno v:
Geological Journal. 55:6544-6561
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b2fb27872d96211cfe3f5bd153d25d53
https://doi.org/10.1002/gj.3821
https://doi.org/10.1002/gj.3821
Autor:
Xi Xu, Hanlin Chen, Andrew V. Zuza, An Yin, Peng Yu, Xiubin Lin, Chongjin Zhao, Juncheng Luo, Shufeng Yang, Baodi Wang
Publikováno v:
Geology. 51:413-413
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::92432a38be1a1213380aadee53e2f3d9
https://doi.org/10.1130/g50615e.1
https://doi.org/10.1130/g50615e.1
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
The Songpan−Aba region is located on the northeastern edge of the Tibetan Plateau. Tectonically, the area is surrounded by the West Qinling orogenic belt in the north, the Longmenshan orogenic belt in the southeast, and the East Kunlun and Sanjiang
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ce93d32c9635b92536469222205bec83
https://doi.org/10.3389/feart.2021.752693
https://doi.org/10.3389/feart.2021.752693
Publikováno v:
GEOPHYSICS. 84:J1-J15
Potential-field sharp-boundary inversion will allow us to identify the sharp petrophysical deposit boundaries inside the host rocks. With the purpose to find a more simple and convenient way to achieve a sharp-boundary and well-focused image for 3D f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9499c7fa383d543bc1c4eb2a0810952e
https://doi.org/10.1190/geo2018-0132.1
https://doi.org/10.1190/geo2018-0132.1