DOI: 10.1007/s00531-017-1456-y
Scopus记录号: 2-s2.0-85014275008
论文题名: Geochronological data of igneous and metamorphic rocks from the Xing’an-Mongolia Orogenic Belt of the eastern Central Asian Orogenic Belt: implications for the final closure of the Paleo-Asian Ocean
作者: Guosheng W. ; Chen W. ; Cheng C. ; Zhiguang Z. ; Changfeng L. ; Tian J.
刊名: International Journal of Earth Sciences
ISSN: 14373254
出版年: 2017
卷: 106, 期: 8 起始页码: 2727
结束页码: 2746
语种: 英语
英文关键词: Erdaojing complex
; Late Paleozoic-Triassic
; Ondor Sum complex
; Paleo-Asian Ocean
; Xing’an-Mongolia Orogenic Belt
Scopus关键词: geochronology
; igneous geochemistry
; metamorphic rock
; metasedimentary rock
; orogenic belt
; paleoceanography
; Paleozoic
; suture zone
; tectonic setting
; Triassic
; uranium-lead dating
; China
; Guangxi Zhuangzu
; Mongolia
; North China Block
; Xingan
英文摘要:
In order to better constrain the evolution of the Xing’an-Mongolia Orogenic Belt and the resulting closure of the Paleo-Asian Ocean, we conducted an integrated investigation involving U-Pb dating of igneous and detrital zircon and a synthesis of existing work across the Erdaojing and Ondor Sum complexes in the eastern segment of the Central Asian Orogenic Belt. Geochronological analysis revealed a different tectonic setting between the Ondor Sum complex (Tulinkai area) and the Erdaojing accretion complex, as detrital zircon U-Pb analysis identified different major age provenances: (1) the Precambrian basement of the North China Craton and Paleozoic Bainaimiao Arc along the northern margin of North China to the south are the provenance rocks of the schists in the Tulinkai area, and (2) the Precambrian basement of the Xilinhot complex and Paleozoic Baolidao arc to the north are the provenance rocks of the schists in the Erdaojing area. We infer that the existence of the ocean between the above two regions in the late of Early Paleozoic in accordance with the result of this study. Furthermore, a comparison of the youngest age population in the intruded-diorite rock and metasedimentary rocks with U-Pb ages implies that the final closure of the Paleo- Asian Ocean along the Solonker Suture Zone most likely occurred in the period between 239 and 222 Ma (Late Paleozoic-Triassic). © 2017, Springer-Verlag Berlin Heidelberg.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-85014275008&doi=10.1007%2fs00531-017-1456-y&partnerID=40&md5=600d492f9bfceb1b621804e25f48f587
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/69935
Appears in Collections: 影响、适应和脆弱性 气候减缓与适应
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作者单位: School of Earth Science and Resources, China University of Geosciences (Beijing), Beijing, China; Sichuan Institute of Geological Engineering Investgation, Chengdu, China
Recommended Citation:
Guosheng W.,Chen W.,Cheng C.,et al. Geochronological data of igneous and metamorphic rocks from the Xing’an-Mongolia Orogenic Belt of the eastern Central Asian Orogenic Belt: implications for the final closure of the Paleo-Asian Ocean[J]. International Journal of Earth Sciences,2017-01-01,106(8)