Zobrazeno 1 - 10
of 39
pro vyhledávání: '"Yi-Can Liu"'
Publikováno v:
Geoscience Frontiers, Vol 9, Iss 4, Pp 1229-1242 (2018)
Ultrahigh-pressure (UHP) metamorphic rocks are distinctive products of crustal deep subduction, and are mainly exposed in continental subduction-collision terranes. UHP slices of continental crust are usually involved in multistage exhumation and par
Externí odkaz:
https://doaj.org/article/3890bd17197348f29738f66016929da6
Publikováno v:
Minerals, Vol 10, Iss 7, p 618 (2020)
The North Dabie complex zone (NDZ), central China, is a high-T ultrahigh-pressure (UHP) metamorphic terrane. It underwent a complex evolution comprising of multistage metamorphism and multiple anatectic events during the Mesozoic continental collisio
Externí odkaz:
https://doaj.org/article/b3f85c402a6a45e2808834e037d6c8c3
Publikováno v:
Minerals, Vol 10, Iss 3, p 213 (2020)
Corundum-bearing anatectic aluminous rocks are exposed in the deeply subducted North Dabie complex zone (NDZ), of Central China. The rocks consist of corundum, biotite, K-feldspar and plagioclase, and show clear macro- and micro-structural evidence o
Externí odkaz:
https://doaj.org/article/93cbca5877514192b0c8606a24e1809b
Publikováno v:
GSA Bulletin. 134:1877-1894
Post-collisional mountain-root collapse and subsequent massive partial melting occurred in the high-temperature (HT) ultrahigh-pressure (UHP) metamorphic terrane of the North Dabie complex zone (NDZ), central China. The NDZ was deeply subducted in th
Publikováno v:
Lithos. :107029
Autor:
Yi-Can Liu, Chengwei Zhang
Publikováno v:
Science China Earth Sciences. 63:1904-1924
The discovery of ultrahigh-pressure (UHP) index minerals such as coesite and micro-diamond in supracrustal rocks indicate that a large amount of crustal rocks were subducted to mantle depths and subsequently returned to the Earth’s surface. However
Publikováno v:
European Journal of Mineralogy. 31:889-903
Autor:
Yi-Can Liu, Yang Yang
Table S1: Electron microprobe analyses (wt%) of representative minerals in the NDZ metadiorites; Table S2: Major and trace elements concentrations of the NDZ metadiorites; Table S3: Zircon SHRIMP U-Pb isotopic compositions of the NDZ metadiorites; Ta
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::07312fb4fb82a97ce1682ae08e721d0a
https://doi.org/10.1130/gsab.s.16859710.v1
https://doi.org/10.1130/gsab.s.16859710.v1
Publikováno v:
Geological Society of America Bulletin. Jul/Aug2022, Vol. 134 Issue 7/8, p1877-1894. 18p.
Publikováno v:
Precambrian Research. 303:268-290
Two types of Paleoproterozoic granitoids, i.e., K-feldspar/albite granites and granitic gneisses, were recognized from the Wuhe Complex of the Precambrian basement and neighboring areas in the southeastern margin of the North China Craton (NCC). They