1-20 OF 125 RESULTS FOR

Panjal Traps

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Series: Geological Society, London, Special Publications
Published: 09 March 2022
DOI: 10.1144/SP518-2020-241
EISBN: 9781786205810
... Abstract Forty-two volcanic rocks of the Panjal Traps were analysed for platinum-group elements (PGEs) to investigate the magma genesis, high-temperature behaviour and exploration potential of these elements. The PGE data exhibit substantial variability and show no systematic relation...
FIGURES | View All (10)
Book Chapter

Series: Geological Society, London, Special Publications
Published: 01 January 2018
DOI: 10.1144/SP463.4
EISBN: 9781786203441
... Abstract: The Early Permian (290 Ma) Panjal Traps are the largest contiguous outcropping of volcanic (basaltic, andesitic and silicic) rocks within the Himalaya that are associated with the Late Palaeozoic break-up of Gondwana. The basaltic Panjal Traps have compositional characteristics...
FIGURES | View All (19)
Journal Article
Published: 01 July 2008
Bulletin de la Société Géologique de France (2008) 179 (4): 383–395.
...François Chauvet; Henriette Lapierre; Delphine Bosch; Stéphane Guillot; Georges Mascle; Jean-Claude Vannay; Jo Cotten; Pierre Brunet; Francine Keller Abstract The late Lower to Middle Permian Panjal Traps (NW Himalaya, India-Pakistan) represent the greatest magmatic province erupted...
FIGURES | View All (8)
Journal Article
Published: 01 July 1981
Geological Magazine (1981) 118 (4): 367–375.
Image
Major and trace elements compositions for the Zanskar-Spiti <span class="search-highlight">Panjal</span> <span class="search-highlight">Traps</span> sa...
Published: 01 July 2008
T able I. – Major and trace elements compositions for the Zanskar-Spiti Panjal Traps samples. T abl . I. – Compositions en éléments majeurs et en éléments traces des échantillons des trapps de Panjal du Zanskar-Spiti.
Image
Geochemical composition of the <span class="search-highlight">Panjal</span> <span class="search-highlight">Traps</span> lavas plots in Mg#, TiO 2 , Y a...
Published: 01 July 2008
F ig . 4. – Geochemical composition of the Panjal Traps lavas plots in Mg#, TiO 2 , Y and Nb/Y vs Zr diagrams. F ig . 4. – Composition géochimique des laves des trapps de Panjal représentée dans les diagrammes de corrélation Mg#, TiO 2 , Y et Nb/Y en fonction de Zr.
Image
Nd, Sr and Pb isotopic compositions of the Zanskar-Spiti <span class="search-highlight">Panjal</span> <span class="search-highlight">Traps</span> sampl...
Published: 01 July 2008
T able IIa. – Nd, Sr and Pb isotopic compositions of the Zanskar-Spiti Panjal Traps samples. T abl . IIa. – Compositions isotopiques du Nd, du Sr et du Pb, des échantillons des trapps de Panjal du Zanskar-Spiti.
Image
Isotopic compositions of the <span class="search-highlight">Panjal</span> <span class="search-highlight">Traps</span> basalts : (a) ( 207 Pb&#x2F; 204 Pb) i...
Published: 01 July 2008
F ig . 6. – Isotopic compositions of the Panjal Traps basalts : (a) ( 207 Pb/ 204 Pb) i vs (206Pb/204Pb) i diagram. (b) (208Pb/204Pb) i vs (206Pb/204Pb) i diagram. (c) εNd i vs (206Pb/204Pb) i diagram. Fields of MORBs are from pre-compiled isotopic compositions in the PETDB (spreading axis
Image
εNd i  vs (Ti&#x2F;Y) plots of the <span class="search-highlight">Panjal</span> <span class="search-highlight">Traps</span> from Zanskar-Spiti (Group 1: bla...
Published: 01 July 2008
F ig . 8. – εNd i vs (Ti/Y) plots of the Panjal Traps from Zanskar-Spiti (Group 1: black squares, Group 2: white squares) and Pakistan (grey circles) [ Spencer et al., 1995] . MORB and OIB values are from Sun and McDonough [1989] and Bulk Crust value is from McLennan [2001] . F ig . 8
Journal Article
Published: 01 February 2017
Italian Journal of Geosciences (2017) 136 (1): 64–72.
... compositions are chondritic and the values of εNd lie between those of MORB and old Indian continental crust. Immobile trace element contents of Stak eclogites are similar to those of the Permian Panjal Traps and significantly different from those of the Deccan Traps erupted at 73–66 Ma in the northwestern...
FIGURES | View All (6)
Image
Present-day εNd values versus MgO diagram for the Stak samples, <span class="search-highlight">Panjal</span> <span class="search-highlight">Trap</span>...
Published: 01 February 2017
Fig. 5 Present-day εNd values versus MgO diagram for the Stak samples, Panjal Traps ( C hauvet et alii , 2008 ; S hellnutt et alii , 2012 ; S hellnutt et alii , 2014 ; S hellnutt et alii , 2015) and pre-Deccan Traps ( M ahoney et alii , 2002 ; K err et al ., 2010 ).
Journal Article
Journal: GSA Bulletin
Published: 01 September 2015
GSA Bulletin (2015) 127 (9-10): 1313–1330.
... and Ta patterns. They were most likely derived from an enriched subcontinental lithospheric mantle source and triggered by the mantle plume–induced rifting process. The Woniusi basaltic province, together with other coeval basaltic provinces from the Panjal Traps, Tethyan Himalaya, Lhasa, and southern...
FIGURES | View All (12)
Series: Geological Society, London, Special Publications
Published: 08 October 2019
DOI: 10.1144/SP483.13
EISBN: 9781786204523
... directly adjacent to the suture zone enclose eclogites of Eocene age, some coesite-bearing (Kaghan/Neelum and Tso Morari), formed from Permian Panjal Trap, continental-type, basaltic magmatic rocks. Eclogites with a granulite-facies overprint, yielding Oligocene–Miocene ages, occur in the anatectic...
FIGURES | View All (19)
Journal Article
Journal: GSA Bulletin
Published: 12 July 2018
GSA Bulletin (2018) 130 (11-12): 2047–2061.
... contiguous plate. Staurolite-grade schists from a higher structural level of the Tanawal Formation record U-Pb monazite ages of ca. 272–267 Ma, indicating the occurrence of Permian regional metamorphism in the area concomitant with major rifting and extrusion of the Panjal Trap volcanics...
FIGURES | View All (7)
Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 June 2013
Lithosphere (2013) 5 (3): 300–320.
... Greater Himalayan Sequence contains two suites of Paleozoic granites: (1) Pan-African Cambrian–Ordovician granites at the cores of gneiss domes and (2) Mississippian–Permian granites related to magmatism associated with the Panjal Traps. Monazite ages record peak through retrograde metamorphic conditions...
FIGURES | View All (17)
Series: Geological Society, London, Special Publications
Published: 01 January 2007
DOI: 10.1144/SP282.15
EISBN: 9781862395305
... small ocean basins, which rifted at more or less the same time in latest Triassic–earliest Jurassic time. All of the rifted margins of the Eastern Tethys are associated with rift-related volcanic rocks. However, with the exception of the Permian Panjal Traps in the Himalayas, the volumes of magma...
FIGURES | View All (39)
Journal Article
Published: 01 January 2001
The Journal of Geology (2001) 109 (1): 127–135.
... that accompanied mafic volcanism (Panjal Trap volcanics) along the north Indian plate margin during rifting of Gondwana. e-mail: srn@nigl.nerc.ac.uk 1 Department of Earth Sciences, Oxford University, Parks Road, Oxford OX1 3PR, United Kingdom. 23 09 1999 29 08 2000 © 2001...
FIGURES | View All (5)
Journal Article
Published: 01 July 1984
Journal of the Geological Society (1984) 141 (4): 763–775.
...-Triassic activity was widespread in terms of both the time interval and area covered. The Abor Volcanic activity in the Eastern Syntaxial Bend of the Himalayan fold belt is coeval with the initiation of Late Carboniferous—Triassic Panjal Trap volcanism of the Western Syntaxial Bend and eruption...
Image
(a) Chondrite– and (b) primitive mantle-normalized [ Sun and McDonough, 198...
Published: 01 July 2008
F ig . 3. – (a) Chondrite– and (b) primitive mantle-normalized [ Sun and McDonough, 1989 ] patterns of the Panjal Traps basalts. F ig . 3. – Composition en éléments traces des basaltes de Panjal : ( a ) Spectres de terres rares normalisés aux chondrites et ( b ) spectres multi-éléments
Image
Location of study area. (A) Reconstruction of Cisuralian paleogeography ( B...
Published: 05 February 2021
Figure 1. Location of study area. (A) Reconstruction of Cisuralian paleogeography ( Boucot et al., 2013 ) showing the study area and major volcanic provinces. PAO—Paleo-Asian Ocean; P—Panjal Traps; S—Skagerrak-Centered large igneous province (LIP); T—Tarim LIP. (B) Locations of study sections