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eastern Pamirs

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Journal Article
Journal: Lithosphere
Published: 16 May 2019
Lithosphere (2019) 11 (4): 560-580.
... and isotopic similarities of units north and south of the Muztaghata gneiss dome, we document the existence of a regionally extensive thrust nappe that stretched across the northern and eastern Pamir, prior to being cut by Miocene exhumation of the Muztaghata dome. The thrust nappe links the Torbashi thrust...
FIGURES | View All (13)
Journal Article
Journal: GSA Bulletin
Published: 01 July 2007
GSA Bulletin (2007) 119 (7-8): 882-896.
... provide new information on the Cenozoic tectonic evolution of the eastern Pamir at the western end of the Himalayan-Tibetan orogen. Field relations and cooling-age patterns in the hanging wall and footwall of the active faults show a southward decrease in the magnitude of east-west extension along...
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Image
Generalized geologic map of the <b>eastern</b> <b>Pamir</b> region noting the location of...
Published: 16 May 2019
Figure 2. Generalized geologic map of the eastern Pamir region noting the location of major Mesozoic and Cenozoic structures. Small circles and triangles (blue—other authors; red—this study) denote the location associated radiometric ages for detrital and igneous zircon samples cited within
Image
Regional geologic map of the <b>eastern</b> <b>Pamir</b>. Map location is shown in  Figur...
Published: 18 April 2018
Figure 2. Regional geologic map of the eastern Pamir. Map location is shown in Figure 1 . The geologic map is compiled from results of this study, Vlasov et al. (1991) , Lindsay (2007) , Burg (2011) , Zanchi and Gaetani (2011) , and Robinson et al. (2004 , 2007 , 2012) . Labeled circles
Image
Geological map of the western Tarim Basin, Kunlun, and <b>eastern</b> <b>Pamir</b> showin...
in > Geosphere
Published: 25 August 2017
Figure 3. Geological map of the western Tarim Basin, Kunlun, and eastern Pamir showing the potential source regions of sediment into the basin. Terrane-bounding faults from Figure 2 are shown in heavier line weight. K—Cretaceous, E.—Early.
Image
Figure 2. Simplified geologic map of the <b>eastern</b> <b>Pamir</b>, northern Karakoram,...
Published: 01 July 2007
Figure 2. Simplified geologic map of the eastern Pamir, northern Karakoram, and Western Kunlun Shan showing distribution of lithologic ages and Cenozoic faults (after Yin and Bian, 1992 ; Strecker et al., 1995 ; Sobel and Dumitru, 1997 ; Robinson et al., 2004 ; Schwab et al., 2004 ). KS—Kudi
Journal Article
Journal: Geology
Published: 01 August 1994
Geology (1994) 22 (8): 707-710.
...M. Brunel; N. Arnaud; P. Tapponnier; Y. Pan; Y. Wang Abstract The northernmost segment of the Karakoram fault is an active normal dextral wrench fault that bounds the Muji-Tashgurgan Pliocene-Quaternary basin (eastern Pamir). The Kongurshan (7719 m) and Mustaghata (7546 m) mountains are interpreted...
Journal Article
Journal: Lithosphere
Published: 01 December 2014
Lithosphere (2014) 6 (6): 443-455.
..., between 15 and −5, for the northeastern Pamir and juvenile to moderately evolved, between 10 and −40, for the central and southern Pamir. Detrital mica 40 Ar/ 39 Ar ages for the northeastern Pamir (eastern drainages) are generally older than ages from the central and southern Pamir (western drainages...
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Journal Article
Journal: Geosphere
Published: 25 August 2017
Geosphere (2017) 13 (5): 1747-1765.
...Figure 3. Geological map of the western Tarim Basin, Kunlun, and eastern Pamir showing the potential source regions of sediment into the basin. Terrane-bounding faults from Figure 2 are shown in heavier line weight. K—Cretaceous, E.—Early. ...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 2014
AAPG Bulletin (2014) 98 (6): 1213-1234.
... reverse faults trending primarily west-northwest and secondarily north–south. The two fault sets are commonly linked to each other by west-northwest-oriented faults bending either southward at their eastern tips or northward at the western tips, and originated possibly from inversion of pre-existing...
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Journal Article
Journal: GSA Bulletin
Published: 30 June 2017
GSA Bulletin (2017) 129 (11-12): 1450-1471.
... fold-and-thrust belt. The western Tajik fold-and-thrust belt records at least 35–40 km of total shortening and is part of the greater Tian Shan orogenic system. The eastern Tajik fold-and-thrust belt records ∼30 km of shortening linked to the Pamir Mountains. The amount of shortening in the Tajik fold...
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Journal Article
Published: 10 August 2018
Journal of the Geological Society (2018) 175 (6): 967-973.
... ratios (0.7118 ± 0.0008, n = 29); and (3) the eastern Pamir Block with diverse values (0.7110 ± 0.0009, n = 19). This map is a promising tool for recognizing the origins of immigrants in the Tarim Basin and may aid understanding of the migration patterns and cultural communication along the Silk Roads...
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Journal Article
Journal: GSA Bulletin
Published: 01 January 2010
GSA Bulletin (2010) 122 (1-2): 145-161.
... system described here extends for ∼350 km along the eastern flank of the Pamir salient. Transpressional right slip along this set of faults, here called the Kashgar-Yecheng transfer system, appears to have accommodated late Cenozoic separation of the North Pamir from the Western Kunlun Shan during south...
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Journal Article
Journal: Lithosphere
Published: 18 April 2018
Lithosphere (2018) 10 (4): 494-511.
...Figure 2. Regional geologic map of the eastern Pamir. Map location is shown in Figure 1 . The geologic map is compiled from results of this study, Vlasov et al. (1991) , Lindsay (2007) , Burg (2011) , Zanchi and Gaetani (2011) , and Robinson et al. (2004 , 2007 , 2012) . Labeled circles...
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Journal Article
Journal: Lithosphere
Published: 23 May 2019
Lithosphere (2019) 11 (4): 507-523.
...., Coutand et al., 2002 ; Li et al., 2012 ; Thompson Jobe et al., 2018 ) ( Fig. 1 ). In the eastern Pamir, the dextral Kashi-Yecheng Transfer System divides the Pamir and the southwestern Tarim Basin ( Fig. 1 ). It has been active in the late Miocene (5–6 Ma) or earliest Pliocene (e.g., Cowgill, 2010...
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Journal Article
Journal: GSA Bulletin
Published: 01 February 2003
GSA Bulletin (2003) 115 (2): 166-181.
...Manfred R. Strecker; George E. Hilley; J Ramón Arrowsmith; Isabelle Coutand Abstract Western, central, and eastern segments of the Trans Alai mountain front in the northern Pamir of Kyrgyzstan have accommodated varying degrees of approachment of the Pamir orogen with respect to the Tien Shan (Shan...
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Journal Article
Journal: Geology
Published: 01 October 2003
Geology (2003) 31 (10): 849-852.
... . Dmitriev , E.A. , 1976 , Kainozoiskie kalievye schelochnye porody Vostochnogo Pamira (Cenozoic potassium rocks of Eastern Pamir) : Dushanbe, Akademiya Nauk Tadzhikskoy SSR , 171 p. (in Russian). Fraser , J.E. , Searle , M.P. , Parrish , R.R. , and Noble , S.R. , 2001...
FIGURES
Journal Article
Journal: GSA Bulletin
Published: 01 July 2004
GSA Bulletin (2004) 116 (7-8): 953-973.
... syntaxis) and central and eastern segments (the Tibetan Plateau) of the Himalayan-Tibetan orogenic belt. The Pamir–western Himalayan syntaxis lies at the western end of the Indo-Asian collision zone and is bounded by the Main Pamir Thrust to the north, and the Main Boundary Thrust and Main Frontal...
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Journal Article
Journal: Geology
Published: 01 December 2014
Geology (2014) 42 (12): 1047-1050.
... : Geological Society of America Bulletin , v. 116 , p. 953 – 973 , doi:10.1130/B25375.1. Robinson A.C. Yin A. Manning C.E. Harrison T.M. Zhang S.H. Wang X.F. , 2007 , Cenozoic evolution of the eastern Pamir: Implications for strain-accommodation mechanisms at the western end...
FIGURES
Series: Geological Society
Published: 01 January 2017
EISBN: 9781862399594
... Shan, is postulated to be underway by c . 20 Ma. Recently published results suggest synchronous strike-slip deformation in the western Tarim Basin and eastern flank of the Pamir. Based on our results and published data, we are able to connect Tarim and Pamir deformation to the onset of TFF slip. We...