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Jaglot Group

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Journal Article
Published: 01 September 1996
Journal of the Geological Society (1996) 153 (5): 681–693.
... the Kamila Amphibolite Belt. Metasediments and basaltic lavas were deposited, within an extensional basin, onto the Kamila Amphibolite Belt basement. This sequence, exposed across the arc, forms a distinct stratigraphic unit which is formally defined here as the Jaglot Group. Sediment-charged turbidity...
Journal Article
Published: 01 September 1998
Journal of the Geological Society (1998) 155 (5): 893–895.
..., increase in metamorphic grade southwards from chloritoid slates in the Hunza valley (developed in the Yasin formation that lies interbedded with the topmost Chalt Volcanics; Pudsey 1986 ) through greenschist-facies rocks (Jaglot group, A. S. Collins, Department of Geology, University of Leicester...
Series: Geological Society, London, Special Publications
Published: 08 October 2019
DOI: 10.1144/SP483.4
EISBN: 9781786204523
... that intrudes the Chalt Volcanic Group, which is, in turn, overlain by the Yasin Group dated at Albian–Aptian ( c. 100–125 Ma) and underlain by the Jaglot Group and Kamila Amphibolites (dated at c . 134 Ma, Khan et al. , 2007, and 95–100 Ma, Anckiewicz & Vance, 2000 respectively). Borneman et al...
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Journal Article
Published: 01 May 2003
Journal of the Geological Society (2003) 160 (3): 377–384.
... geochemical signature ( Fig. 3 ) and forms part of the volcanic sequence of the juvenile arc. The Jaglot Group immediately overlies the Kamila Amphibolites, although, in the east, the contact is masked by the intrusive Chilas Complex ( Fig. 2 ). Rocks of the Jaglot Group contain both pillowed and massive...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2010
DOI: 10.1144/SP338.14
EISBN: 9781862395862
... Amphibolites; (3) Jijal Complex lower crustal–mantle arc-root; (4) Jaglot Group sediments and volcanic rocks; (5) Chalt volcanic rocks,; (6) Kohistan batholith stage 1 plus Yasin sediments; (7) Chilas Complex; (8) Kohistan batholith stage 2; (9) Dir Group and Shamran/Teru volcanic rocks; (10) Kohistan...
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Journal Article
Published: 01 June 1982
Journal of the Geological Society (1982) 139 (3): 299–308.
... @ 1982 The Geological Society 300 M. P. Coward et al. Map Area g R , PlNDl KARACH U BOOkm 50 km 8 Thrust. teeth on hanglng wall 4 Ywnglng dlrectlon f Fold plunge and dlrectlon - Jaglot syncllne and assoclated folds Pre-Jaglot age antlcllne In Chllas complex 5 Follatlan Murree formatlon I Mlocene...
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.170.01.04
EISBN: 9781862394186
... units to the Kohistan arc. The nearest possible correlatives are the metasediments of the Jaglot Group ( Treloar et al. 1996 ). The protolith to these strata are greywackes with intercalated basalts and volcaniclastic sediments. However, the Raikhot strata described here have substantial calcareous...
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Journal Article
Published: 01 June 1987
Journal of the Geological Society (1987) 144 (3): 377–391.
...). It is clear that the northern suture, the major upright folds in Kohistan, the decoupling zone in amphibolite facies rocks along the Indus river near Jaglot, the folds and fabrics in the Chilas complex and much of the deformation in the Kamila amphibolite group must be of Cretaceous age, post-dating the early...
Journal Article
Published: 01 December 1997
Journal of the Geological Society (1997) 154 (6): 935–946.
... Kohistan arc began in Early Cretaceous time (Yasin Group carbonates of Aptian Albian age; Pudsey 1986), consistent with Ar/Ar and Rb/Sr ages indicating that the bulk of the igneous infrastructure formed between 110 and 90 Ma (Schärer et al. 1984; Petterson & Windley 1985; Treloar et al. 1989...