Zobrazeno 1 - 10
of 16
pro vyhledávání: '"Zewei YAO"'
Autor:
Zewei Yao
Publikováno v:
Applied Sciences, Vol 14, Iss 19, p 8621 (2024)
Host rock deformation associated with sill emplacement is used to constrain magma transfer and storage within the upper crust. In contrast to classic models suggesting that the host rock above mafic sills is dominated by elastic bending, recent studi
Externí odkaz:
https://doaj.org/article/c24fdd9cdd0b487aab79f8e8df385589
Autor:
Zewei Yao
Publikováno v:
Minerals, Vol 14, Iss 9, p 862 (2024)
Interpretation of the seismic reflection profiles associated with borehole data from the petroleum industry offers a novel way to study sill emplacement in sedimentary basins. This study uses this approach to reveal the intrusive part of the Tarim La
Externí odkaz:
https://doaj.org/article/cd1a1f8f91fb465b9b6b38f2820301a7
Autor:
Guangyu HE, Yongqiang ZHAO, Zewei YAO, Xiaoli ZHENG, Sidong XIAO, Jiwen HUANG, Cunshan JIA, Yushuang ZHOU
Publikováno v:
Shiyou shiyan dizhi, Vol 42, Iss 6, Pp 886-891 (2020)
The Wensu Uplift is an important structural belt in the northern Tarim Basin, NW China, always regarded as a thrust belt. However, this recognition is not only incompatible with the facts that synthetic and antithetic faults are equally developed in
Externí odkaz:
https://doaj.org/article/51c9a9e326804e2e83a6197e914f069c
Autor:
Guangyu HE, Yi GU, Yongqiang ZHAO, Zewei YAO, Xiaoli ZHENG, Sidong XIAO, Jiwen HUANG, Cunshan JIA, Yushuang ZHOU
Publikováno v:
Shiyou shiyan dizhi, Vol 42, Iss 2, Pp 172-176 (2020)
The Shaya Uplift, an important structural belt in the northern Tarim Basin, northwestern China, has been regarded as a thrust belt. However, this recognition is not only incompatible with the flower structures on the seismic profiles, but also contra
Externí odkaz:
https://doaj.org/article/a929569be72e432296556be668682939
Publikováno v:
Applied Sciences, Vol 12, Iss 20, p 10553 (2022)
Recently, many studies have been conducted on the stratum deformation induced by earth pressure balance (EPB) shield tunneling in soft soil and sand. Movement laws vary largely among different strata. However, at present, relevant research mainly foc
Externí odkaz:
https://doaj.org/article/69155a4448e34c98b12f96785c78f514
Autor:
Gang Li, Aqeel Abbas, Xi Peng, Zewei Yao, Xuelin Qiu, Xiaoli Wan, Yutao Liu, Yonglin Wen, Chun-Feng Li, Jia-zheng Zhang
Publikováno v:
Geophysical Journal International. 225:811-828
SUMMARYThe post-spreading magmatic activities in the northeastern South China Sea (SCS) margin are very strong, evidenced by widely distributed high-velocity lower crust (HVLC) and numerous volcanoes. However, there are large contrasts in magmatic ac
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::44fb890a32e149fb06c0dc4c2bf2e7b7
https://doi.org/10.1093/gji/ggab006
https://doi.org/10.1093/gji/ggab006
Publikováno v:
IEEE Internet of Things Journal. :1-1
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7bf7e1d24b7950c09eaea63d67cc98b5
https://doi.org/10.1109/jiot.2023.3272010
https://doi.org/10.1109/jiot.2023.3272010
Publikováno v:
Earth and Planetary Science Letters. 501:37-45
Igneous sills are widely distributed in sedimentary basins worldwide. Sill emplacement has significant impacts on structural and thermal evolutions of sedimentary basins and also provides important insights into volcanic and sub-volcanic processes. D
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e6867d96b0cb93de06d352f5114ed77f
https://doi.org/10.1016/j.epsl.2018.08.026
https://doi.org/10.1016/j.epsl.2018.08.026
Publikováno v:
Marine and Petroleum Geology. 133:105255
The transition from continental to oceanic crust and the initial formation of typical oceanic crust at passive rifted margin are still poorly understood. In this study, deep crustal structures in the transitional domain of the northeastern South Chin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a1635be6bee0d51fda6500c4d3222f9f
https://doi.org/10.1016/j.marpetgeo.2021.105255
https://doi.org/10.1016/j.marpetgeo.2021.105255