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Sutlej Valley

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Journal Article

Tectonic implications of Palaeoproterozoic anatexis and Late Miocene metamorphism in the Lesser Himalayan Sequence, Sutlej Valley, NW India Available to Purchase

J.A. CHAMBERS, T.W. ARGLES, M.S.A. HORSTWOOD, N.B.W. HARRIS, R.R. PARRISH, T. AHMAD
Published: 01 May 2008
Journal of the Geological Society (2008) 165 (3): 725–737.
DOI: https://doi.org/10.1144/0016-76492007/090
... in apatite and zircon fission-track data, indicating faster exhumation of the Wangtu Gneiss Complex (hanging wall) compared with the Jutogh metasediments (footwall) during the Plio-Pleistocene. However, this contrast in exhumation rates is not clear from other fission-track studies based in the Sutlej Valley...
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View PDF for article title, Tectonic implications of Palaeoproterozoic anatexis and Late Miocene metamorphism in the Lesser Himalayan Sequence, <span class="search-highlight">Sutlej</span> <span class="search-highlight">Valley</span>, NW India
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Journal Article

Randon/Helium Survey of Thermal Springs of Parbati, Beas and Sutlej Valleys in Himachal Himalaya Available to Purchase

H. S. Virk, Anand K. Sharma, Naresh Kumar
Published: 01 November 1998
Jour. Geol. Soc. India (1998) 52 (5): 523–528.
DOI: https://doi.org/10.17491/jgsi/1998/520503
... JOURNAL GEOLOGICAL SOCIETY OF INDIA Vo1.52, Nov. 1998, pp.523-528 R.adonlH:elium Survey of Thermal Springs of 1?arbati, Beas and Sutlej Valleys in Himachal Himalaya H.S.VIRK, ANAND K. SHARMA and NARESH KUMAR Department of Physics, Guru Nanak Dev University, .A'Idntsar - 143005 '11 Abstract: India has...
View PDF for article title, Randon&#x2F;Helium Survey of Thermal Springs of Parbati, Beas and <span class="search-highlight">Sutlej</span> <span class="search-highlight">Valleys</span> in Himachal Himalaya
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Image
The geological map of the Sutlej valley, NW Himalaya (after Vannay et al., 2004; Thakur and Patel, 2012). (a) Inset showing regional map of the Himalaya, (b) Inset showing a generalized N-S cross-section of the Himalaya, and (c) sample locations of mafic xenoliths.

The geological map of the Sutlej valley, NW Himalaya (after Vannay et al.,... Available to Purchase

Published: 01 June 2017
Fig.1. The geological map of the Sutlej valley, NW Himalaya (after Vannay et al., 2004 ; Thakur and Patel, 2012 ). (a) Inset showing regional map of the Himalaya, (b) Inset showing a generalized N-S cross-section of the Himalaya, and (c) sample locations of mafic xenoliths.
Image
 (a) Geological sketch map of a section of the Sutlej Valley after Caddick et al. (2007), based on Vannay et al. (1999), with modifications from our field observations. Jutogh Group localities (sample set ‘JC I05’) marked by diamonds (leucogranites), triangles (metasediments) and squares (sheared amphibolite); ‘W60’ from Richards et al. (2005). Line A–A′ marks the location of the cross-section in (b). GHS, Greater Himalayan Sequence; LHS, Lesser Himalayan Sequence; STD, South Tibetan Detachment; VT, Vaikrita Thrust; KD, Karcham Detachment; ST, Sarahan Thrust; MT, Munsiari Thrust; CT, Chail Thrust. (b) Cross-section with detailed foliation trajectories projected onto the line of section A–A′ in (a) from field measurements. (c) Simplified geological sketch map showing stretching lineations and metamorphic isograds. grt, garnet; st, staurolite; ky, kyanite; sill, sillimanite; mig, migmatite.

( a ) Geological sketch map of a section of the Sutlej Valley after Caddic... Available to Purchase

Published: 01 May 2008
Fig. 2.  ( a ) Geological sketch map of a section of the Sutlej Valley after Caddick et al . (2007) , based on Vannay et al . (1999) , with modifications from our field observations. Jutogh Group localities (sample set ‘JC I05’) marked by diamonds (leucogranites), triangles (metasediments
Image
Figure 2. Photograph of the alluvial infill in the lower Sutlej Valley, taken from the eastern part of Figure 1 toward the southwest. The Sutlej River is flowing to the upper part of the picture

Figure 2. Photograph of the alluvial infill in the lower Sutlej Valley, tak... Available to Purchase

Published: 01 July 2006
Figure 2. Photograph of the alluvial infill in the lower Sutlej Valley, taken from the eastern part of Figure 1 toward the southwest. The Sutlej River is flowing to the upper part of the picture
Journal Article

Holocene monsoonal dynamics and fluvial terrace formation in the northwest Himalaya, India Available to Purchase

B. Bookhagen, D. Fleitmann, K. Nishiizumi, M.R. Strecker, R.C. Thiede
Journal: Geology
Published: 01 July 2006
Geology (2006) 34 (7): 601–604.
DOI: https://doi.org/10.1130/G22698.1
...Figure 2. Photograph of the alluvial infill in the lower Sutlej Valley, taken from the eastern part of Figure 1 toward the southwest. The Sutlej River is flowing to the upper part of the picture ...
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View PDF for article title, Holocene monsoonal dynamics and fluvial terrace formation in the northwest Himalaya, India
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Journal Article

Zircon geochronology and Hf isotopic study from the Leo Pargil Dome, India: implications for the palaeogeographic reconstruction and tectonic evolution of a Himalayan gneiss dome Available to Purchase

Shashi Ranjan Rai, Himanshu K. Sachan, Christopher J. Spencer, Aditya Kharya, Saurabh Singhal, Arun Kumar Ojha, Pallavi Chattopadhaya, Pitambar Pati
Published: 11 July 2022
Geological Magazine (2022) 159 (10): 1681–1698.
DOI: https://doi.org/10.1017/S0016756822000449
...Shashi Ranjan Rai; Himanshu K. Sachan; Christopher J. Spencer; Aditya Kharya; Saurabh Singhal; Arun Kumar Ojha; Pallavi Chattopadhaya; Pitambar Pati Abstract U–Pb geochronology, Hf isotopes and trace-element chemistry of zircon grains from migmatite of the upper Sutlej valley (Leo Pargil...
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View PDF for article title, Zircon geochronology and Hf isotopic study from the Leo Pargil Dome, India: implications for the palaeogeographic reconstruction and tectonic evolution of a Himalayan gneiss dome
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Book Chapter

SHRIMP U–Pb c . 1860 Ma anorogenic magmatic signatures from the NW Himalaya: implications for Palaeoproterozoic assembly of the Columbia Supercontinent Available to Purchase

Author(s)
Sandeep Singh, A. K. Jain, Mark E. Barley
Book: Palaeoproterozoic Supercontinents and Global Evolution
Series: Geological Society, London, Special Publications
Publisher: The Geological Society of London
Published: 01 January 2009
DOI: 10.1144/SP323.14
EISBN: 9781862395718
... ages from Bandal granitoids, Kulu–Bajura mylonite and Wangtu granitoids along the Sutlej Valley, Himachal Pradesh. Some of the zircon crystals contain older cores mostly extending back to 2600 Ma. We report for the first time a 3000 Ma old zircon core from Wangtu granitoids, which indicates reworking...
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Abstract
View PDF for content titled, SHRIMP U–Pb c . 1860 Ma anorogenic magmatic signatures from the NW Himalaya: implications for Palaeoproterozoic assembly of the Columbia Supercontinent
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Abstract The basal parts of the Higher Himalayan Crystallines (HHC), Lesser Himalayan sedimentary sequences and mylonite zone at the base of Main Central Thrust (MCT) within the NW Himalaya clearly demonstrate anorogenic magmatic signatures at around 1860 Ma, as indicated by SHRIMP U–Pb zircon ages from Bandal granitoids, Kulu–Bajura mylonite and Wangtu granitoids along the Sutlej Valley, Himachal Pradesh. Some of the zircon crystals contain older cores mostly extending back to 2600 Ma. We report for the first time a 3000 Ma old zircon core from Wangtu granitoids, which indicates reworking of ensialic Archaean crust during the assembly of the Columbia Supercontinent between 2.1 and 1.8 Ga. During the Himalayan collisional tectonics, the reworked Archaean and Palaeoproterozoic crust was imbricated and placed adjacent to each other in the Higher Himalayan Crystallines, the Inner Lesser Himalayan window zone and the Kulu–Bajura Nappe.

Journal Article

Late Quaternary intensified monsoon phases control landscape evolution in the northwest Himalaya Available to Purchase

Bodo Bookhagen, Rasmus C. Thiede, Manfred R. Strecker
Journal: Geology
Published: 01 February 2005
Geology (2005) 33 (2): 149–152.
DOI: https://doi.org/10.1130/G20982.1
... movements. Here we use lacustrine deposits related to spatially and temporally clustered large landslides (>0.5 km 3 ) in the Sutlej Valley region of the northwest Himalaya to calculate sedimentation rates and to infer rainfall patterns during late Pleistocene (29–24 ka) and Holocene (10–4 ka...
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Image
Field photographs of the Main Central thrust (MCT) zone and its hanging wall (locations marked in Figs. 6A–6C). (A) Baragaon gneiss, mylonitized in the MCT zone along the Sutlej River. (B) Folded concordant contact of Baragaon gneiss with Haimanta schist, Sutlej River Valley. (C) Isoclinal folds of Haimanta quartzite and phyllite; foliation is preferentially developed in the pelitic layers, Beas River Valley. (D) Mylonitization of the base of the Mandi granite, near Karsog. (E) Bulk of the Mandi granite is weakly deformed to undeformed; photo from near Mandi. (F) Brittle faulting and folding near Rohru. (G) Isoclinal folding of the Greater Himalayan Crystalline complex in Tos Valley. (H) Tight folds in the Greater Himalayan Crystalline complex, Chandra Valley. (I) Shear bands in the Greater Himalayan Crystalline complex, Sutlej Valley.

Field photographs of the Main Central thrust (MCT) zone and its hanging wal... Open Access

Published: 01 August 2011
Figure 8. Field photographs of the Main Central thrust (MCT) zone and its hanging wall (locations marked in Figs. 6A–6C ). (A) Baragaon gneiss, mylonitized in the MCT zone along the Sutlej River. (B) Folded concordant contact of Baragaon gneiss with Haimanta schist, Sutlej River Valley. (C
Image
Field photographs of the Main Central thrust (MCT) zone and its hanging wall (locations marked in Figs. 6A–6C). (A) Baragaon gneiss, mylonitized in the MCT zone along the Sutlej River. (B) Folded concordant contact of Baragaon gneiss with Haimanta schist, Sutlej River Valley. (C) Isoclinal folds of Haimanta quartzite and phyllite; foliation is preferentially developed in the pelitic layers, Beas River Valley. (D) Mylonitization of the base of the Mandi granite, near Karsog. (E) Bulk of the Mandi granite is weakly deformed to undeformed; photo from near Mandi. (F) Brittle faulting and folding near Rohru. (G) Isoclinal folding of the Greater Himalayan Crystalline complex in Tos Valley. (H) Tight folds in the Greater Himalayan Crystalline complex, Chandra Valley. (I) Shear bands in the Greater Himalayan Crystalline complex, Sutlej Valley.

Field photographs of the Main Central thrust (MCT) zone and its hanging wal... Open Access

Published: 01 August 2011
Figure 8. Field photographs of the Main Central thrust (MCT) zone and its hanging wall (locations marked in Figs. 6A–6C ). (A) Baragaon gneiss, mylonitized in the MCT zone along the Sutlej River. (B) Folded concordant contact of Baragaon gneiss with Haimanta schist, Sutlej River Valley. (C
Image
Field photographs of the Main Central thrust (MCT) zone and its hanging wall (locations marked in Figs. 6A–6C). (A) Baragaon gneiss, mylonitized in the MCT zone along the Sutlej River. (B) Folded concordant contact of Baragaon gneiss with Haimanta schist, Sutlej River Valley. (C) Isoclinal folds of Haimanta quartzite and phyllite; foliation is preferentially developed in the pelitic layers, Beas River Valley. (D) Mylonitization of the base of the Mandi granite, near Karsog. (E) Bulk of the Mandi granite is weakly deformed to undeformed; photo from near Mandi. (F) Brittle faulting and folding near Rohru. (G) Isoclinal folding of the Greater Himalayan Crystalline complex in Tos Valley. (H) Tight folds in the Greater Himalayan Crystalline complex, Chandra Valley. (I) Shear bands in the Greater Himalayan Crystalline complex, Sutlej Valley.

Field photographs of the Main Central thrust (MCT) zone and its hanging wal... Open Access

Published: 01 August 2011
Figure 8. Field photographs of the Main Central thrust (MCT) zone and its hanging wall (locations marked in Figs. 6A–6C ). (A) Baragaon gneiss, mylonitized in the MCT zone along the Sutlej River. (B) Folded concordant contact of Baragaon gneiss with Haimanta schist, Sutlej River Valley. (C
Image
Field photographs of the Main Central thrust (MCT) zone and its hanging wall (locations marked in Figs. 6A–6C). (A) Baragaon gneiss, mylonitized in the MCT zone along the Sutlej River. (B) Folded concordant contact of Baragaon gneiss with Haimanta schist, Sutlej River Valley. (C) Isoclinal folds of Haimanta quartzite and phyllite; foliation is preferentially developed in the pelitic layers, Beas River Valley. (D) Mylonitization of the base of the Mandi granite, near Karsog. (E) Bulk of the Mandi granite is weakly deformed to undeformed; photo from near Mandi. (F) Brittle faulting and folding near Rohru. (G) Isoclinal folding of the Greater Himalayan Crystalline complex in Tos Valley. (H) Tight folds in the Greater Himalayan Crystalline complex, Chandra Valley. (I) Shear bands in the Greater Himalayan Crystalline complex, Sutlej Valley.

Field photographs of the Main Central thrust (MCT) zone and its hanging wal... Open Access

Published: 01 August 2011
Figure 8. Field photographs of the Main Central thrust (MCT) zone and its hanging wall (locations marked in Figs. 6A–6C ). (A) Baragaon gneiss, mylonitized in the MCT zone along the Sutlej River. (B) Folded concordant contact of Baragaon gneiss with Haimanta schist, Sutlej River Valley. (C
Image
Field photographs of the Main Central thrust (MCT) zone and its hanging wall (locations marked in Figs. 6A–6C). (A) Baragaon gneiss, mylonitized in the MCT zone along the Sutlej River. (B) Folded concordant contact of Baragaon gneiss with Haimanta schist, Sutlej River Valley. (C) Isoclinal folds of Haimanta quartzite and phyllite; foliation is preferentially developed in the pelitic layers, Beas River Valley. (D) Mylonitization of the base of the Mandi granite, near Karsog. (E) Bulk of the Mandi granite is weakly deformed to undeformed; photo from near Mandi. (F) Brittle faulting and folding near Rohru. (G) Isoclinal folding of the Greater Himalayan Crystalline complex in Tos Valley. (H) Tight folds in the Greater Himalayan Crystalline complex, Chandra Valley. (I) Shear bands in the Greater Himalayan Crystalline complex, Sutlej Valley.

Field photographs of the Main Central thrust (MCT) zone and its hanging wal... Open Access

Published: 01 August 2011
Figure 8. Field photographs of the Main Central thrust (MCT) zone and its hanging wall (locations marked in Figs. 6A–6C ). (A) Baragaon gneiss, mylonitized in the MCT zone along the Sutlej River. (B) Folded concordant contact of Baragaon gneiss with Haimanta schist, Sutlej River Valley. (C
Image
Field photographs of the Main Central thrust (MCT) zone and its hanging wall (locations marked in Figs. 6A–6C). (A) Baragaon gneiss, mylonitized in the MCT zone along the Sutlej River. (B) Folded concordant contact of Baragaon gneiss with Haimanta schist, Sutlej River Valley. (C) Isoclinal folds of Haimanta quartzite and phyllite; foliation is preferentially developed in the pelitic layers, Beas River Valley. (D) Mylonitization of the base of the Mandi granite, near Karsog. (E) Bulk of the Mandi granite is weakly deformed to undeformed; photo from near Mandi. (F) Brittle faulting and folding near Rohru. (G) Isoclinal folding of the Greater Himalayan Crystalline complex in Tos Valley. (H) Tight folds in the Greater Himalayan Crystalline complex, Chandra Valley. (I) Shear bands in the Greater Himalayan Crystalline complex, Sutlej Valley.

Field photographs of the Main Central thrust (MCT) zone and its hanging wal... Open Access

Published: 01 August 2011
Figure 8. Field photographs of the Main Central thrust (MCT) zone and its hanging wall (locations marked in Figs. 6A–6C ). (A) Baragaon gneiss, mylonitized in the MCT zone along the Sutlej River. (B) Folded concordant contact of Baragaon gneiss with Haimanta schist, Sutlej River Valley. (C
Image
Field photographs of the Main Central thrust (MCT) zone and its hanging wall (locations marked in Figs. 6A–6C). (A) Baragaon gneiss, mylonitized in the MCT zone along the Sutlej River. (B) Folded concordant contact of Baragaon gneiss with Haimanta schist, Sutlej River Valley. (C) Isoclinal folds of Haimanta quartzite and phyllite; foliation is preferentially developed in the pelitic layers, Beas River Valley. (D) Mylonitization of the base of the Mandi granite, near Karsog. (E) Bulk of the Mandi granite is weakly deformed to undeformed; photo from near Mandi. (F) Brittle faulting and folding near Rohru. (G) Isoclinal folding of the Greater Himalayan Crystalline complex in Tos Valley. (H) Tight folds in the Greater Himalayan Crystalline complex, Chandra Valley. (I) Shear bands in the Greater Himalayan Crystalline complex, Sutlej Valley.

Field photographs of the Main Central thrust (MCT) zone and its hanging wal... Open Access

Published: 01 August 2011
Figure 8. Field photographs of the Main Central thrust (MCT) zone and its hanging wall (locations marked in Figs. 6A–6C ). (A) Baragaon gneiss, mylonitized in the MCT zone along the Sutlej River. (B) Folded concordant contact of Baragaon gneiss with Haimanta schist, Sutlej River Valley. (C
Image
Field photographs of the Main Central thrust (MCT) zone and its hanging wall (locations marked in Figs. 6A–6C). (A) Baragaon gneiss, mylonitized in the MCT zone along the Sutlej River. (B) Folded concordant contact of Baragaon gneiss with Haimanta schist, Sutlej River Valley. (C) Isoclinal folds of Haimanta quartzite and phyllite; foliation is preferentially developed in the pelitic layers, Beas River Valley. (D) Mylonitization of the base of the Mandi granite, near Karsog. (E) Bulk of the Mandi granite is weakly deformed to undeformed; photo from near Mandi. (F) Brittle faulting and folding near Rohru. (G) Isoclinal folding of the Greater Himalayan Crystalline complex in Tos Valley. (H) Tight folds in the Greater Himalayan Crystalline complex, Chandra Valley. (I) Shear bands in the Greater Himalayan Crystalline complex, Sutlej Valley.

Field photographs of the Main Central thrust (MCT) zone and its hanging wal... Open Access

Published: 01 August 2011
Figure 8. Field photographs of the Main Central thrust (MCT) zone and its hanging wall (locations marked in Figs. 6A–6C ). (A) Baragaon gneiss, mylonitized in the MCT zone along the Sutlej River. (B) Folded concordant contact of Baragaon gneiss with Haimanta schist, Sutlej River Valley. (C
Image
Field photographs of the Main Central thrust (MCT) zone and its hanging wall (locations marked in Figs. 6A–6C). (A) Baragaon gneiss, mylonitized in the MCT zone along the Sutlej River. (B) Folded concordant contact of Baragaon gneiss with Haimanta schist, Sutlej River Valley. (C) Isoclinal folds of Haimanta quartzite and phyllite; foliation is preferentially developed in the pelitic layers, Beas River Valley. (D) Mylonitization of the base of the Mandi granite, near Karsog. (E) Bulk of the Mandi granite is weakly deformed to undeformed; photo from near Mandi. (F) Brittle faulting and folding near Rohru. (G) Isoclinal folding of the Greater Himalayan Crystalline complex in Tos Valley. (H) Tight folds in the Greater Himalayan Crystalline complex, Chandra Valley. (I) Shear bands in the Greater Himalayan Crystalline complex, Sutlej Valley.

Field photographs of the Main Central thrust (MCT) zone and its hanging wal... Open Access

Published: 01 August 2011
Figure 8. Field photographs of the Main Central thrust (MCT) zone and its hanging wall (locations marked in Figs. 6A–6C ). (A) Baragaon gneiss, mylonitized in the MCT zone along the Sutlej River. (B) Folded concordant contact of Baragaon gneiss with Haimanta schist, Sutlej River Valley. (C
Image
Field photographs showing the development of in situ melt along the late extensional crenulation cleavage (ECC) from (a) Sikkim Himalaya of Eastern Himalaya, (b) Sutlej Valley, and (c) Bhagirathi Valley of NW Himalaya

Field photographs showing the development of in situ melt along the late ... Available to Purchase

Published: 01 January 2023
Fig.2. Field photographs showing the development of in situ melt along the late extensional crenulation cleavage (ECC) from (a) Sikkim Himalaya of Eastern Himalaya, (b) Sutlej Valley, and (c) Bhagirathi Valley of NW Himalaya
Image
 Tectonostratigraphic column across the metamorphic core exposed in the Sutlej Valley. Not to scale. Abbreviations as for Figure 2; and chl, chlorite; bi, biotite.

Tectonostratigraphic column across the metamorphic core exposed in the Sutl... Available to Purchase

Published: 01 May 2008
Fig. 3.  Tectonostratigraphic column across the metamorphic core exposed in the Sutlej Valley. Not to scale. Abbreviations as for Figure 2 ; and chl, chlorite; bi, biotite.