Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Mingjin Hou"'
Publikováno v:
Solid Earth Sciences, Vol 6, Iss 2, Pp 205-227 (2021)
The Zhangbaling tectonic belt is located in the middle segment of Dabie-Sulu Orogenic Belt and in the eastern part of the main segment of the Tan-Lu Fault Zone (TLFZ). Based on detailed field work and comprehensive analysis, this study discussed the
Externí odkaz:
https://doaj.org/article/eac85e3d540a419d9c4d0a22183716f8
Publikováno v:
Solid Earth Sciences, Vol 6, Iss 2, Pp 205-227 (2021)
The Zhangbaling tectonic belt is located in the middle segment of Dabie-Sulu Orogenic Belt and in the eastern part of the main segment of the Tan-Lu Fault Zone (TLFZ). Based on detailed field work and comprehensive analysis, this study discussed the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d4c1dc10dd538e400229402c7adbf703
http://www.sciencedirect.com/science/article/pii/S2451912X20300313
http://www.sciencedirect.com/science/article/pii/S2451912X20300313
Publikováno v:
Journal of Asian Earth Sciences. 25:601-609
This paper presents new geological data from the Lantian area of Anhui Province, SE China, that contradict the hypothesis of the Lantian tectonic window—one of the key argument in Hsu's Mesozoic collision tectonic model for south China. The 1:50,00
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1544b6937731fb9084634e4ecb1f38b1
https://doi.org/10.1016/j.jseaes.2004.05.007
https://doi.org/10.1016/j.jseaes.2004.05.007
Publikováno v:
Scopus-Elsevier
The southern and northern parts of the eastern margin of the Jiangnan Upheaval, located in the northeast of Jiangxi Province (Gandongbei) and the south of Anhui Province (Wannan) share many similar...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2c71e4d75707630597e66f2f5c0bda7f
https://doi.org/10.1080/10020070412331344841
https://doi.org/10.1080/10020070412331344841
Publikováno v:
Chinese Science Bulletin. 42:1726-1729
1. The eclogite dikes in low-greenschist facies epi-metamorphic volcaniclastic rocks in the Dabie Mountains areas show magma origin rather than tectonic melange or metamorphic origin. 2. Coesite and quartz pseudomorphs in the eclogite show that they
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b930cd5b8bf439e18d32b23177a09f6e
https://doi.org/10.1007/bf02882676
https://doi.org/10.1007/bf02882676
Publikováno v:
Acta Geologica Sinica (English Edition); Apr2004, Vol. 78 Issue 2, p380-386, 7p
Autor:
Taofa, Zhou1 tfzhou@hiut.edu.cn, Feng, Yuan1, Mingjin, Hou2, Yü, Fan1, Jianguo, Du2, Guang, Zhu1, Shucang, Yue1
Publikováno v:
Progress in Natural Science. Dec2004, Vol. 14 Issue 12, p1080-1087. 8p.