Zobrazeno 1 - 10
of 55
pro vyhledávání: '"Guangying, Feng"'
Publikováno v:
Geological Magazine. :1-24
In the Late Neoarchaean, the lithosphere of the North China Craton (NCC) experienced a strong extensional event, which is of great significance for understanding the evolution of the continental crust in the Precambrian. In this study, a suite of maf
Autor:
Jing-Gui Sun, Shen Liu, Guangying Feng, Jingyan Xu, Ian M. Coulson, Huibo Zhao, Xiaoqing Chen, Yan Fan, Caixia Feng
Publikováno v:
Acta Geologica Sinica - English Edition. 95:419-438
Publikováno v:
The Journal of Geology. 128:535-562
Ophiolites in the southern belt (SB) occur as much larger peridotite massifs compared with those of the northern belt (NB), sporadically overlain by a thin layer of isotropic gabbro in the ...
Autor:
Xiangzhen Xu, Basem Zoheir, Jingsui Yang, Fahui Xiong, Guolin Guo, Guangying Feng, Zhaoli Li, Tianfu Li
Publikováno v:
Lithos. :106947
Publikováno v:
Lithos. :106924
Publikováno v:
Geological Magazine. 158:158-174
We report new U–Pb zircon age data, zircon in situ oxygen isotope, mineral chemistry, whole-rock geochemistry and Sr–Nd isotopic compositions from the Early Devonian ultrapotassic Gucheng pluton in the North China Craton, and discuss its petrogen
Publikováno v:
The Journal of Geology. 127:61-79
The North China Craton (NCC) witnessed major extensional tectonic events at the close of the Neoarchean with anorogenic magmatic pulses, which have important implications for understanding ...
Publikováno v:
Geological Magazine. 158:143-157
The Zhangguangcai Range in the Xing’an Mongolian Orogenic Belt, NE China, contains Early Jurassic (c. 188 Ma) Dabaizigou (DBZG) porphyritic dolerite. Compared with other island-arc mafic rocks, the DBZG dolerite is characterized by high trace-eleme
Autor:
Shen Liu, M. Santosh, Zhuang Guo, Hao Peng, Guangying Feng, Mengjing Xu, Qiang Feng, Ian M. Coulson, Xiaolei Guo, Caixia Feng
Publikováno v:
Journal of Geodynamics. 114:19-40
Evolution of the lithospheric mantle beneath the North China Craton (NCC) from its Precambrian cratonic architecture until Paleozoic, and the transformation to an oceanic realm during Mesozoic, with implications on the destruction of cratonic root ha
Autor:
Caixia Feng, Xiaolei Guo, Ian M. Coulson, Shen Liu, Guangying Feng, Hao Peng, Qiang Feng, Zhuang Guo, Mengjing Xu
Publikováno v:
Journal of Geodynamics. 109:41-58
Six mafic dyke swarms crop out in Hebei Province within the Taihang-Da Hinggan gravity lineament magmatic belt, China, and were sampled. Here, we present new zircon laser ablation-inductively coupled plasma-mass spectrometry U-Pb age, whole rock geoc