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Jian Zhang
Sun Yat-sen University
11Publications
4H-index
89Citations
Publications 11
Newest
Published on Apr 1, 2019in Lithos 3.86
Jiahui Qian3
Estimated H-index: 3
(Sun Yat-sen University),
Changqing Yin5
Estimated H-index: 5
(Sun Yat-sen University)
+ 1 AuthorsJian Zhang4
Estimated H-index: 4
(Sun Yat-sen University)
Abstract The Zhujiafang ductile shear zone is located in the central Hengshan Complex, a key area for understanding the Paleoproterozoic tectonic evolution of the Trans-North China Orogen, North China Craton. Detailed metamorphic and geochronological analyses were carried out on metapelite and garnet amphibolite from the Zhujiafang ductile shear zone. The metapelite preserves two phases of mineral assemblages: early kyanite-rutile-bearing assemblage and late chlorite-staurolite-bearing assemblag...
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Published on Mar 12, 2019in Acta Geologica Sinica-english Edition 2.51
Jin Liu2
Estimated H-index: 2
(Sun Yat-sen University),
Jian Zhang4
Estimated H-index: 4
(Sun Yat-sen University)
+ 5 AuthorsMiao Yazhou (Sun Yat-sen University)
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Published on Nov 1, 2018in Lithos 3.86
Luojuan Wang3
Estimated H-index: 3
(Sun Yat-sen University),
Jinghui Guo47
Estimated H-index: 47
(Chinese Academy of Sciences)
+ 4 AuthorsJiahui Qian3
Estimated H-index: 3
(Sun Yat-sen University)
Abstract The Liangcheng garnet granitoids are parautochthonous S-type granites that occur within granulite-facies metasediments in the ultrahigh-temperature (UHT) Jining Complex, eastern part of the Khondalite Belt, North China Craton. These garnet granitoids contain mafic microgranular enclaves and are intimately associated with numerous small intrusions of the Xuwujia gabbronorites, showing magma mingling and mixing textures. Typical mineralogy in the garnet granitoids is plagioclase + K-felds...
1 Citations Source Cite
Published on Jun 1, 2018in Precambrian Research 3.91
Jin Liu2
Estimated H-index: 2
(Sun Yat-sen University),
Jian Zhang4
Estimated H-index: 4
(Sun Yat-sen University)
+ 5 AuthorsShiyong Dou2
Estimated H-index: 2
Abstract The tectonic evolution of the Jiao-Liao-Ji Belt (JLJB) has been a hot topic into understanding the Precambrian geology of the North China Craton. Although there is a broad consensus that the JLJB is a Paleoproterozoic mobile belt, whether it has experienced a rift-and-collision or a simply arc-continental collision event still remains controversial. The Central JLJB preserves excellent rock exposures of variable ages and therefore represents the most promising area to tackle the above c...
5 Citations Source Cite
Published on Jun 1, 2018in Journal of Asian Earth Sciences 2.87
Jin Liu2
Estimated H-index: 2
(Sun Yat-sen University),
Jian Zhang4
Estimated H-index: 4
(Sun Yat-sen University)
+ 3 AuthorsYoubo Peng2
Estimated H-index: 2
Abstract At the junction between the North China Craton (NCC) and the Central Asian Orogenic Belt (CAOB), northern Liaoning province, NE China, there are widespread Jurassic igneous rocks. The tectonic setting and petrogenesis of these rocks are unresolved. Zircon U–Pb dating, whole-rock geochemistry, and Hf isotopic compositions of Jurassic granitoids were investigated to constrain their ages and petrogenesis in order to understand the tectonic evolution of the Paleo-Pacific Ocean along the nor...
2 Citations Source Cite
Published on Apr 1, 2018in Journal of Asian Earth Sciences 2.87
Jiahui Qian3
Estimated H-index: 3
(Sun Yat-sen University),
Changqing Yin5
Estimated H-index: 5
(Sun Yat-sen University)
+ 2 AuthorsLuojuan Wang3
Estimated H-index: 3
(Sun Yat-sen University)
Abstract Mafic granulites in the Fuping Complex occur as lenses or boudins within high-grade TTG (Trondhjemite–Tonalite–Granodiorite) gneisses. Petrographic observations reveal four generations of mineral assemblage in the granulites: an inclusion assemblage of hornblende + plagioclase + ilmenite + quartz within garnet core; an inferred peak assemblage composed of garnet ± hornblende + plagioclase + clinopyroxene + rutile/ilmenite + quartz; a decompression assemblage characterized by symplectite...
3 Citations Source Cite
Published on Dec 1, 2017in Precambrian Research 3.91
Fulai Liu21
Estimated H-index: 21
,
Jian Zhang4
Estimated H-index: 4
(Sun Yat-sen University),
Chaohui Liu17
Estimated H-index: 17
Abstract As one of representative cratons in China, the North China Craton records a long-term and complicated tectonic history, including the formation of Eoarchean continental nucleus, Neoarchean continental crustal growth and reworking, Paleoproterozoic amalgamation of micro-blocks and formation of orogenic belts related to the Columbia supercontinent, and formation of late Paleoproterozoic to early Neoproterozoic rifts. In recent years, extensive geochemical, geochronological, magmatic and m...
4 Citations Source Cite
Published on Sep 1, 2017in Precambrian Research 3.91
Wenjing Li2
Estimated H-index: 2
(Sun Yat-sen University),
Changqing Yin5
Estimated H-index: 5
(Sun Yat-sen University)
+ 3 AuthorsLuojuan Wang3
Estimated H-index: 3
(Sun Yat-sen University)
Abstract The Khondalite Belt is a Paleoproterozoic tectonic belt in the Western Block of the North China Craton. It consists mainly of high-grade metamorphosed Al-rich sedimentary rocks, also named as the ‘Khondalite Series’. The vast majority of detrital zircons from the Khondalite Series rocks have ages dominantly at 2.2–2.0 Ga, but their provenances become an enigma due to lack of available synchronous magmatic rocks. In this paper, detailed geochronological and geochemical studies were done ...
3 Citations Source Cite
Published on Jul 1, 2017in Precambrian Research 3.91
Jun Hong Zhao1
Estimated H-index: 1
(China University of Geosciences),
Paul D. Asimow38
Estimated H-index: 38
(California Institute of Technology)
+ 3 AuthorsJianping Zheng38
Estimated H-index: 38
(China University of Geosciences)
The configuration of the supercontinent Rodinia has long been a matter of debate; the key controversy is the position of South China in Rodinia. We report an incomplete Neoproterozoic ophiolite sequence, including gabbros and serpentinized peridotites intruded by mafic dikes, near Shimian (Sichuan Province), along the western margin of the Yangtze Block in South China. Serpentinized peridotites have very low REE (0.14–1.16 ppm) and trace element concentrations, and are interpreted as parts of a ...
6 Citations Source Cite
Published on Oct 1, 2016in Precambrian Research 3.91
Boran Guo11
Estimated H-index: 11
(Peking University),
LIUShuwen36
Estimated H-index: 36
(Peking University)
+ 3 AuthorsMaojiang Wang6
Estimated H-index: 6
(Peking University)
Abstract The Jiapigou granite-greenstone belt of Southern Jilin Province is located at the northeastern margin of the North China Craton (NCC). The Neoarchean metavolcanic rocks of this region provide strong lines of evidence in petrology and geochemistry for Neoarchean crust–mantle geodynamic evolution and significant crustal growth events. The metavolcanic rock assemblage is dominated by amphibolite, hornblende/garnet biotite plagioclase gneiss, and minor felsic gneiss. Zircon LA–ICP–MS U–Pb i...
29 Citations Source Cite
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