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Nindam Formation

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Figure 3. Structural cross sections through the <b>Nindam</b> <b>Formation</b> showing th...
Published: 01 March 2000
Figure 3. Structural cross sections through the Nindam Formation showing the tectonic relationship of the Nindam Formation with surrounding units and the general north-vergent sense of motion. Location of profiles is shown in Figure 2 .
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Figure 4. Lithologic log of the base of the <b>Nindam</b> <b>Formation</b> in the Zanskar...
Published: 01 March 2000
Figure 4. Lithologic log of the base of the Nindam Formation in the Zanskar Gorge where thrusting has preserved the top of igneous basement.
Journal Article
Journal: GSA Bulletin
Published: 01 March 2000
GSA Bulletin (2000) 112 (3): 450–466.
...Figure 3. Structural cross sections through the Nindam Formation showing the tectonic relationship of the Nindam Formation with surrounding units and the general north-vergent sense of motion. Location of profiles is shown in Figure 2 . ...
FIGURES | View All (15)
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TABLE 2. Nd ISOTOPIC DATA FROM THE <b>NINDAM</b> AND NAKTUL <b>FORMATIONS</b>
Published: 01 March 2000
TABLE 2. Nd ISOTOPIC DATA FROM THE NINDAM AND NAKTUL FORMATIONS
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Figure 11. Spider diagrams of the <b>Nindam</b> and Naktul <b>Formations</b>, normalized ...
Published: 01 March 2000
Figure 11. Spider diagrams of the Nindam and Naktul Formations, normalized against normal mid-oceanic ridge basalt (MORB) ( Sun and McDonough, 1989 ). Water-mobile elements are on the left side of figure; water-immobile elements are on the right. Compatibility in mantle phases increases toward
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TABLE 1. CHEMICAL COMPOSITIONS OF SEDIMENTARY ROCKS FROM THE <b>NINDAM</b> AND NAK...
Published: 01 March 2000
TABLE 1. CHEMICAL COMPOSITIONS OF SEDIMENTARY ROCKS FROM THE NINDAM AND NAKTUL FORMATIONS
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Figure 10. Chondrite-normalized rare earth element diagrams for the <b>Nindam</b> ...
Published: 01 March 2000
Figure 10. Chondrite-normalized rare earth element diagrams for the Nindam and Naktul Formations. Dras volcanic data are from Deitrich et al. (1983) . Mariana volcaniclastic data are from Clift and Lee (1998) .
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Figure 14. Nd isotopic range measured in samples from the <b>Nindam</b> and Naktul...
Published: 01 March 2000
Figure 14. Nd isotopic range measured in samples from the Nindam and Naktul Formations compared with measured values from the High Himalaya ( Allègre and Ben Othman, 1980 ; Searle et al., 1997 ), Trans-Himalaya ( Allègre and Rousseau, 1988 ), and Kohistan ( Khan et al., 1997 ). N-MORB—normal mid
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Figure 9. Rose diagrams showing the direction of paleocurrent flow along th...
Published: 01 March 2000
Figure 9. Rose diagrams showing the direction of paleocurrent flow along three separate sections of the Nindam Formation.
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Figure 6. Sedimentary logs, recorded bed by bed, showing typical exposures ...
Published: 01 March 2000
Figure 6. Sedimentary logs, recorded bed by bed, showing typical exposures of fine-grained, distal turbidites within the Nindam Formation.
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.170.01.19
EISBN: 9781862394186
... zones are connected by a narrow (<500m) strand of sheared serpentinite mélange, 30 km long, which separates the volcanic-sedimentary Naktul unit in the west from the volcaniclastic Nindam Formation in the east (both units of the Dras arc complex). As far as is known, this cross-cutting serpentinitic...
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Figure 12. Ce/Y plotted against Zr/Nb ( Latin et al., 1990 ), showing the s...
Published: 01 March 2000
Figure 12. Ce/Y plotted against Zr/Nb ( Latin et al., 1990 ), showing the similarity of the Nindam Formation and the Chalt and Jutal Groups associated with intraoceanic subduction. There is a contrast with the higher Ce/Y values of the Late Cretaceous–Paleocene Kardung Volcanic Group erupted during
Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 23 March 2018
Lithosphere (2018) 10 (3): 446–459.
..., 1996 ; Dupuis et al., 2005 , 2006 ; Ji et al., 2009 ; Wu et al., 2010 ; Aitchison et al., 2011 ; Cai et al., 2012 ; Wang et al., 2012 ; An et al., 2014 , 2017 ). Notably less has been done to identify trench deposits, with the exception of the Nindam Formation in the Ladakh Himalaya, India...
FIGURES | View All (7)
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2013
DOI: 10.1144/SP372.20
EISBN: 9781862396357
... Cretaceous Nindam Formation, which was deposited in a forearc setting in the Ladakh Himalayas ( Clift et al. 2000 ). However, these volcaniclastic sediments are significantly more depleted in TiO 2 , consistent with their inferred intra-oceanic setting (Fig. 15 ). Based on the petrographic study...
FIGURES | View All (23)
Journal Article
Journal: GSA Bulletin
Published: 01 July 2005
GSA Bulletin (2005) 117 (7-8): 902–925.
...Peter D. Clift; Amy E. Draut; Peter B. Kelemen; Jerzy Blusztajn; Andrew Greene Abstract The Early Jurassic Talkeetna Volcanic Formation forms the upper stratigraphic level of an oceanic volcanic arc complex within the Peninsular Terrane of south-central Alaska. The section comprises a series...
FIGURES | View All (18)
Journal Article
Published: 01 May 2004
Journal of Micropalaeontology (2004) 23 (1): 3–9.
...SUNIL BAJPAI; ROBIN C. WHATLEY; G.V.R. PRASAD; JOHN E. WHITTAKER Abstract A small fauna of three species of non-marine cypridacean Ostracoda has been recovered from the Basgo Formation of the Ladakh Molasse in the North Western Himalaya, India. All three species are new and are described herein...
FIGURES
Journal Article
Published: 01 March 2006
Journal of Sedimentary Research (2006) 76 (3): 493–514.
... Formation of south-central Alaska, and introduce new data from the Mariana Arc, to produce a conceptual model of volcaniclastic sedimentation processes in oceanic arc settings. All three arcs are interpreted to have formed in tectonically erosive margin settings, resulting in long-term extension...
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Ternary diagrams showing the petrographic composition of turbiditic sandsto...
Published: 23 March 2018
—volcanic; Ls—sedimentary). Data for the Nindam Formation and mélange from Garzanti and Van Haver (1988) and for the Rongmawa Formation from Cai et al. (2012) .
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Figure 5. Schematic log showing variation in dominant lithology over sectio...
Published: 01 March 2000
Figure 5. Schematic log showing variation in dominant lithology over section lengths of 10 m and greater. The figure demonstrates the overall variation in sedimentary lithology in the Nindam Formation within the Yapola Gorge section. Location is shown in Figure 2 . Black—fine-grain–dominated
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2002
DOI: 10.1144/GSL.SP.2002.195.01.07
EISBN: 9781862394438
... forearc is exposed towards the south. The Cretaceous Nindam Formation represents the forearc basin to an oceanic volcanic island arc (Dras-Kohistan Arc) accreted to the margin of Eurasia ( Cannat & Mascle 1990 ; Steck et al. 1993 ; Robertson & Degnan 1994 ; Clift et al. 2000a ). Although...