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Ganmachidam Formation

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Journal Article
Published: 01 February 1978
Jour. Geol. Soc. India (1978) 19 (2): 73–78.
... the EurydesmaDeltopecten is not considered as glacial by Nakazawa et al (1975). Similarly in Spiti and also in the present area the Ganmachidam Formation of the Kanawar Group (Srikantia, 1974), which underlies the Kuling Formation, does not contain any character of glacial environment (Bhargava and Bhattacharyya, 1975...
Journal Article
Published: 01 June 1998
Jour. Geol. Soc. India (1998) 51 (6): 777–784.
.... The Haimanta Group in Zanskar consisting of Batal, Kunzum La and Thango Formations is overlain by the Kanawar group (Srikantia et a1. 1978) which is divided into Lipak, Po, and Ganmachidam Formations. Kanwar Group directly overlaps the Thango Formation in most of Zanskar Basin particularly in the NW side...
Journal Article
Published: 01 September 1977
Jour. Geol. Soc. India (1977) 18 (9): 509–511.
...S. V. Srikantia; T. M. Ganesan; P. K. Sinha; B. Tirkey Copyright © 1977 Geological Society of India 1977 Geological Society of India A note on the significance of granite clasts in a diamictite of the Thango Formation (Lower Silurian) Zanskar valley, Ladakh Himalaya S. V. SRIKANTJA, T. M...
Journal Article
Published: 01 September 2011
Journal of Sedimentary Research (2011) 81 (9): 702–707.
... – 119 . Garzanti , E. , Angiolini , L. , and Sciunnach , D. 1996 , The Mid-Carboniferous to lowermost Permian succession of Spiti (Po Group and Ganmachidam Formation; Tethys Himalaya, northern India): Gondwana glaciation and rifting of Neo-Tethys : Geodinamica Acta , v. 9 , p. 78...
FIGURES
Series: Geological Society, London, Special Publications
Published: 31 March 2023
DOI: 10.1144/SP515-2020-108
EISBN: 9781786205872
... and Ganmachidam formations ( Table 1 ). As the Lipak Formation has a conformable and gradational contact with the underlying Muth Formation, the Muth Formation was also placed in the Kanawar Group ( Bhargava 2008 ). The age of the Kanawar Group ranges from Late Devonian to Permo-Carboniferous. Muth Formation...
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Book Chapter

Series: Text Book
Published: 01 January 2021
DOI: 10.17491/bgsi.2021.9857.06
EISBN: 9789380998572
..., 3. Batal Formation (Haimanta Group), 4. Kunzam La Formation (Haimanta Group), 5. Thango and Takche formations (Sanugba Group), 6. Muth Formation (Kanawar Group), 7. Lipak Formation (Kanawar Group), 8. Po Formation (Kanawar Group), 9. Ganmachidam Formation (Kanawar Group), 10. Kuling Group, l0a...
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Journal Article
Published: 01 January 2023
Jour. Geol. Soc. India (2023) 99 (1): 61–64.
... of Jaisalmer Basin . Petroleum Asia Jour. , v. 2 (1) , pp. 106 – 128 . Singh , B.P. , Bhargava , O.N. , Mikuláš , R. , Prasad , S.K. , Singla , G. and Kaur , R. (2017) Asteriacites and other trace fossils from the Po Formation (Visean-Serpukhovian), Ganmachidam Hill, Spiti...
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Book Chapter

Published: 01 January 2010
DOI: 10.17491/bgsi.2010.9865.01
EISBN: 978-93-80998-65-7
... by Lipak, Po and Ganmachidam Formations. Further SE they continue into Spiti-Kinnaur segment of the larger Spiti-Zanskar sub-basin. Eastern Karakoram The Karakoram Range is a NW-SE trending orogenic belt extending within Hunza and northern Ladakh area of Jammu and Kashmir. Geologically it comprises...
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Journal Article
Published: 01 November 1979
Jour. Geol. Soc. India (1979) 20 (11): 531–539.
...S. V. Srikantia; O. N. Bhargava Abstract The Tandi Group of Lahaul area in the Himachal Higher Himalaya represents a sequence of essentially carbonate rocks. It is underlain by chlorite phyllite representing possibly metamorphosed lava flows and overlies Precambrian-Eocambrian Batal Formation...
Journal Article
Published: 01 June 1995
Jour. Geol. Soc. India (1995) 45 (6): 629–642.
... Group, 3. Batal Formation (Haimanta Group), 4. Kunzam La Formation (Haimanta Group), 5. Thange Formation (Haimanta Group), 6. Much and Takche Formations, 7. Lipak Formation (Kanawar Group), 8. Po Formation (Kanawar Group), 9. Ganmachidam Formation (Kanawar Group), 10. Kuling ~ormatibn1, 0a. Chlorite phy...
Journal Article
Published: 01 November 2005
Geological Magazine (2005) 142 (6): 765–781.
... . Garzanti , E. , Angiolini , L. & Sciunnach , D. 1996b . The Mid-Carboniferous to lowermost Permian succession of Spiti (Po Group and Ganmachidam Formation; Tethys Himalaya, Northern India): Gondwana glaciation and rifting of Neo-Tethys . Geodinamica Acta 9 , 78 – 100...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 2007
GeoArabia (2007) 12 (3): 35–56.
... and Ganmachidam Formation ; Tethys Himalaya, Northern India): Gondwana glaciation and rifting of Neo-Tethys. Geodinamica Acta , v. 9 , p. 78 – 100 . Garzanti , E. , L. Angiolini and D. Sciunnach 1996b . The Permian Kuling Group (Spiti...
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Book Chapter

Series: Text Book
Published: 01 January 2021
DOI: 10.17491/bgsi.2021.9857.03
EISBN: 9789380998572
... (Tournasian) in age. The succeeding Po Formation with its arenite-shale sequence is Lower to Lower-Middle Carboniferous. The Ganmachidam has a gradational contact with the Po and is characterised by conglomerate lenses of varying size and is Upper Carboniferous to earliest Permian (?) in age. It had shallow...
Journal Article
Journal: PALAIOS
Published: 01 April 2001
PALAIOS (2001) 16 (2): 126–147.
.... , and Sciunnach , D. , 1996 . The Mid-Carboniferous to lowermost Permian succession of Spiti (Po Group and Ganmachidam Formation; Tethys Himalaya, Northern India): Gondwana glaciation and rifting of Neo-Tethys : Geodinamica Acta , v. 9 , p. 78 – 100 . Gerdes , G. , Klenke , T. , and Noffke...
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Journal Article
Published: 14 April 2020
Journal of the Geological Society (2020) 177 (4): 866–881.
... ( Tantiwanit et al . 1983 ; Stauffer and Lee 1986 ; Raksaskulwong and Wongsowanich 1993 ; Ampaiwan et al . 2009 ). The CIA values of the studied mudrocks are similar to those of glacial diamictites in the Ganmachidam Formation in India (average CIA = 60), which was located at 40–45°S in the early Permian...
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Book Chapter

Published: 01 January 2010
EISBN: 978-93-80998-65-7
... Ganga (Ganges) Plain, 957 Gangamopteris Beds, 601, 650 Gangapur Formation, 630, 641 Ganmachidam Formation, 565, 597 Garbyang Formation, 582, 589 Garhwal-Kumaun Tethyan sub-basin, 561 Garu Formation, 607 Garudamangalam Formation, 715 Gauran Beds, 585 Gauss, 833...
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 2009
GeoArabia (2009) 14 (4): 17–48.
...) . Journal of Geophysical Research , v. 105 , no. B2 , p. 2805 – 2815 . Garzanti , E. , L. Angiolini and D. Sciunnach 1996 . The mid–Carboniferous to lowermost Permian succession of Spiti (Po Group and Ganmachidam Formation; Tethys...
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Journal Article
Published: 01 July 2008
Bulletin de la Société Géologique de France (2008) 179 (4): 383–395.
... the Alpine chains. Today, preserved fragments of those margins carry traces of the different within-plate magmatic episodes, which accompanied their formation. The latter are dispersed along the Tethyan orogenic belt (fig. 1a ), from Australia, Himalaya, Oman, to Zagros and eastern Mediterranean chains...
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Journal Article
Published: 01 October 2022
Italian Journal of Geosciences (2022) 141 (3): 400–425.
.... ( 2017 ) - Asteriacites and other trace fossils from the Po Formation (Visean–Serpukhovian), Ganmachidam Hill, Spiti Valley (Himalaya) and its paleoenvironmental significance . Geol. Carpath. , 68 , 464 – 478 . https://doi.org/10.1515/geoca-2017-0030 . Smith A. , Braddy S.J...
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Book Chapter

Series: SEPM Concepts in Sedimentology and Paleontology
Published: 01 January 2013
DOI: 10.2110/sepmcsp.11.126
EISBN: 9781565762893
... the Rangit Pebble Slate (T95: 27°N, 92°E, T96: 27°N, 93.5°E; T97: 27°N, 95.5°E; see also Singh, 1993 ). Srikantia et al. (1979) cited diamictite in the Ganmachidam Formation (T98: 34°N, 78°E). The Tethyan Asselian Agglomeratic Slate of Kashmir is cited by Wopfner and Casshyap (1997) (T99: 34°N, 75°E...
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