2003
DOI: 10.1130/0016-7606(2003)115<0881:dgotnt>2.0.co;2
|View full text |Cite
|
Sign up to set email alerts
|

Detrital-zircon geochronology of the northeastern Tibetan plateau

Abstract: Detrital-zircon geochronology of the northeastern Tibetan plateau Email alerting services cite this article to receive free e-mail alerts when new articles www.gsapubs.org/cgi/alerts click Subscribe America Bulletin to subscribe to Geological Society of www.gsapubs.org/subscriptions/ click Permission request to contact GSA http://www.geosociety.org/pubs/copyrt.htm#gsa click viewpoint. Opinions presented in this publication do not reflect official positions of the Society. positions by scientists worldwide, reg… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
2
1

Citation Types

9
279
0
5

Year Published

2007
2007
2023
2023

Publication Types

Select...
6
1

Relationship

0
7

Authors

Journals

citations
Cited by 367 publications
(293 citation statements)
references
References 24 publications
9
279
0
5
Order By: Relevance
“…(1) A north-facing arc, which is interpreted to have brought the Nan Shan-Qilian Shan-Altun Shan terrane juxtaposed with the southern margin of the Tarim craton (Yin and Nie, 1996;Sobel and Arnaud, 1999;Gehrels et al, 2003aGehrels et al, , 2003b (Fig. 10a).…”
Section: Tectonic Implicationsmentioning
confidence: 99%
“…(1) A north-facing arc, which is interpreted to have brought the Nan Shan-Qilian Shan-Altun Shan terrane juxtaposed with the southern margin of the Tarim craton (Yin and Nie, 1996;Sobel and Arnaud, 1999;Gehrels et al, 2003aGehrels et al, , 2003b (Fig. 10a).…”
Section: Tectonic Implicationsmentioning
confidence: 99%
“…The late Paleoproterozoic to Neoproterozoic detritalzircon grains in the analyzed samples were probably derived from the Central Qilian Block, where Mesoproterozoic-Neoproterozoic granitic intrusions and metamorphosed sedimentary rocks with late Paleoproterozoic to Neoproterozoic detrital zircons constitute the major part of the basement ( fig. 9e, 9f; Guo et al 2000;Wan et al 2001;Gehrels et al 2003aGehrels et al , 2003bTung et al 2007a;Wang et al 2007;Xu et al 2007;Yong et al 2008a;Xue et al 2009). Cambrian-Ordovician zircon grains, in addition to Precambrian detritus, occur in the Lujiaogou Formation of the Sunan area in the Sunan Subprovince ) and in the Late Ordovician sediments of Xiehao area in the Jingyuan Subprovince (Xu et al 2010; fig.…”
Section: Resultsmentioning
confidence: 99%
“…Potential ophiolitic source rocks within the North Qilian Belt are represented by the Jiugequan, Dachadaban, and Yushigou-Dongcaohe ophiolites, which were emplaced during the Cambrian to Early-Middle Ordovician within/between the back (Xu et al 2010); e, Central Qilian Block granitic intrusions (Guo et al 2000;Wan et al 2000Wan et al , 2001Gehrels et al 2003b;Tung et al 2007a;Wang et al 2007;Xu et al 2007;Yong et al 2008a;Xue et al 2009); f, metasedimentary basement of the Central Qilian Block (Gehrels et al 2003a;Tung et al 2007a;Xu et al 2007); g, detrital zircons from the basement of the North China Craton (Krö ner et al 1988;Wan et al 2003;Darby and Gehrels 2006;Tung et al 2007b;Li et al 2008 (Xia et al 2003) and the high-Crcontent rocks of the Dachadaban ophiolite (Chen et al 1995;Zhang et al 1998b). The average value of Shuiquan samples, representing the continent provenances ), was calculated with Dachadaban ophioliteprovenance average value to generate two-end-member mixing lines, accounting for the high Cr/Th and Cr/V ratios of some samples from the Lujiaogou Formation.…”
Section: Resultsmentioning
confidence: 99%
See 2 more Smart Citations