Zobrazeno 1 - 10
of 27
pro vyhledávání: '"Xianglin Qian"'
Publikováno v:
In Gondwana Research 1999 2(4):568-571
Publikováno v:
Gondwana Research. 14:395-409
Remnants of 2.1–1.8 Ga orogens can be recognized in nearly every craton assembled within reconstructions of the Rodinia supercontinent, although no particular pattern of laterally extensive orogenic belts emerges. These cratons may be the fragments
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::44b1b4a50d27a05a05eb6512bde6ca24
https://doi.org/10.1016/j.gr.2008.01.010
https://doi.org/10.1016/j.gr.2008.01.010
Publikováno v:
Gondwana Research. 14:561-566
The 1.3– 1.2 Ga fan- shaped Mackenzie dyke swarm and other similar- aged dyke swarms in the Canadian Shield constitute the subswarms of a Late Mesoproterozoic giant radiating swarm. The Late Mesoproterozoic mafic dyke swarms in Australia and East A
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::67e6321eafeca8b75b7fa422a555bcc0
https://doi.org/10.1016/j.gr.2008.03.005
https://doi.org/10.1016/j.gr.2008.03.005
Publikováno v:
Tectonophysics. 422:89-98
Mafic dyke swarms and aulacogens are major anorogenic extensional events in the Late Paleoproterozoic North China Craton (NCC). The N–NNW mafic dyke swarms are widespread in the NCC, whose ages span between 1.83 and 1.77 Ga. The similar ages and or
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7351974ebf6a731e63d802b919968947
https://doi.org/10.1016/j.tecto.2006.05.008
https://doi.org/10.1016/j.tecto.2006.05.008
Publikováno v:
Geophysical Journal International. 143:185-203
A palaeomagnetic pole position, derived from a precisely dated primary remanence, with minimal uncertainties due to secular variation and structural correction, has been obtained for China’s largest dyke swarm, which trends for about 1000 km in a N
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2ea86e89e44b10f3be616027be07716f
https://doi.org/10.1046/j.1365-246x.2000.00231.x
https://doi.org/10.1046/j.1365-246x.2000.00231.x
Publikováno v:
Science in China Series D: Earth Sciences. 43:253-265
Within the high-grade metamorphic basement, the central portion of North China Craton (NCC), a group of Neoarchean khondalites (KS) is identified. They are characterized by large ion lithophile elements (LILE) enrichment, lower abundances of Zr, Hf a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e39e9e59c9129ded33a40aeaefd6cf46
https://doi.org/10.1007/bf02906821
https://doi.org/10.1007/bf02906821
Autor:
Qihan Shen, Xianglin Qian
Publikováno v:
Episodes. 18:44-48
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::da3e413c164807731e2e0c914306153b
https://doi.org/10.18814/epiiugs/1995/v18i1.2/010
https://doi.org/10.18814/epiiugs/1995/v18i1.2/010
Publikováno v:
Journal of the Virtual Explorer. 37
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ea0af14ae903ad1c6ba5a67252bbb840
https://doi.org/10.3809/jvirtex.2011.00257
https://doi.org/10.3809/jvirtex.2011.00257
Publikováno v:
Precambrian Research. 59:207-223
The dominant rock types in the khondalite suite in the Archean to Early Proterozoic granulite belt of north-central China are sillimanite-garnet gneiss (SGG), quartz-garnet gneiss (QGG), and quartz-feldspar gneiss (QFG). Field and geochemical results
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6fddb31f310924ad939b7c87f993908d
https://doi.org/10.1016/0301-9268(92)90057-u
https://doi.org/10.1016/0301-9268(92)90057-u
Publikováno v:
Journal of the Virtual Explorer. 22
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::234df511ad5f3f91ff2d79996e385052
https://doi.org/10.3809/jvirtex.2006.00148
https://doi.org/10.3809/jvirtex.2006.00148