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  • 1
    Online Resource
    Online Resource
    Tectonics of the deccan large igneous province (2017)
    London : The Geological Society
    Details Availability
    Keywords: Deccan traps ; Geology, Structural ; Deccan traps ; Geology, Structural ; India ; Deccan ; Dekhan ; Ergussgestein ; Vulkanismus ; Geologie ; Tektonik ; Aufsatzsammlung ; Trapp ; Gang ; Morphotektonik ; Neotektonik ; Rift ; Seismotektonik ; Vulkanische Decke ; Riftsystem
    Description / Table of Contents: Tectonics of the Deccan Large Igneous Province: an introduction /Soumyajit Mukherjee, Achyuta Ayan Misra, Gérôme Calvès and Michal Nemčok --Deccan Plateau uplift: insights from parts of Western Uplands, Maharashtra, India /Vivek S. Kale, Gauri Dole, Devdutt Upasani and Shilpa Patil Pillai --Alteration and submergence of basalts in Kachchh, Gujarat, India: implications for the role of the Deccan Traps in the India-Seychelles break-up /Souvik Mitra, Kaushik Mitra, Saibal Gupta, Satadru Bhattacharya, Prakash Chauhan and Nirmala Jain --Tectonomagmatic setting of lava packages in the Mandla lobe of the eastern Deccan volcanic province, India: palaeomagnetism and magnetostratigraphic evidence /Vamdev Pathak, S. K. Patil and J. P. Shrivastava --Rift-drift transition in a magma-rich system: the Gop Rift-Laxmi Basin case study, West India /M. Nemčok and S. Rybár --Subsidence around oceanic ridges along passive margins: NE Arabian Sea /Achyuta Ayan Misra, Smita Banerjee, Nishikanta Kundu and Brunti Mukherjee --Investigations of continued reservoir triggered seismicity at Koyna, India /Harsh K. Gupta, Kusumita Arora, N. Purnachandra Rao, Sukanta Roy, V. M. Tiwari, Prasanta K. Patro, H. V. S. Satyanarayana, D. Shashidhar, C. R. Mahato, K. N. S. S. S. Srinivas, M. Srihari, N. Satyavani, Y. Srinu, D. Gopinadh, Haris Raza, Monikuntala Jana, Vyasulu V. Akkiraju, Deepjyoti Goswami, Digant Vyas, C. P. Dubey, D. Ch. V. Raju, Ujjal Borah, Kashi Raju, K. Chinna Reddy, Narendra Babu, B. K. Bansal and Shailesh Nayak --Influence of Deccan volcanism/synrift magmatism on the crust-mantle structure and its implications for the seismogenesis of earthquakes occurring in the Kachchh rift zone /Prantik Mandal
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (363 Seiten) , Illustrationen
    ISBN: 9781786203281 , 1786203286
    Series Statement: Geological Society special publication no. 445
    URL: http://sp.lyellcollection.org/content/445/1
    URL: https://geoscienceworld.org/books/book/2020
    URL: https://sp.lyellcollection.org/content/445/1
    URL: https://doi.org/10.1144/SP445
    DOI: 10.1144/SP445
    DDC: 555.48
    Language: English
    Note: Includes bibliographical references and index
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  • 2
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    (Table 1) Lithology of sediment core PAK-G2
    PANGAEA
    Details
    Publication Date: 2023-05-12
    Keywords: AGE; Arabian Sea; Carbonates; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; Lithology/composition/facies; PAK-G2; Sand; Sediment thickness; Silt; Size fraction 〈 0.002 mm, clay
    Type: Dataset
    Format: text/tab-separated-values, 91 data points
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    DATA PANGAEA
  • 3
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    Lithology of sediments from the Arabian Sea
    PANGAEA
    In:  Supplement to: Calves, Gerome; Clift, Peter D; Inam, Asif (2008): Anomalous subsidence on the rifted volcanic margin of Pakistan: No influence from Deccan plume. Earth and Planetary Science Letters, 272(1-2), 231-239, https://doi.org/10.1016/j.epsl.2008.04.042
    Details
    Publication Date: 2023-06-27
    Description: The role of hotter than ambient plume mantle in the formation of a rifted volcanic margin in the northern Arabian Sea is investigated using subsidence analysis of a drill site located on the seismically defined Somnath volcanic ridge. The ridge has experienced 〉4 km of subsidence since 65 Ma and lies within oceanic lithosphere. We estimate crustal thickness to be 9.5-11.5 km. Curiously 〈400 m of the thermal subsidence occurred prior to 37 Ma, when subsidence rates would normally be at a maximum. We reject the hypothesis that this was caused by increasing plume dynamic support after continental break-up because the size of the thermal anomalies required are unrealistic (〉600°C), especially considering the rapid northward drift of India relative to the Deccan-Réunion hotspot. We suggest that this reflects very slow lithospheric growth, possibly caused by vigorous asthenospheric convection lasting 〉28 m.y., and induced by the steep continent-ocean boundary. Post-rift slow subsidence is also recognized on volcanic margins in the NE Atlantic and SE Newfoundland and cannot be used as a unique indicator of plume mantle involvement in continental break-up.
    Keywords: 24-237; Arabian Sea; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Indian Ocean//PLATEAU; Leg24; PAK-G2
    Type: Dataset
    Format: application/zip, 2 datasets
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    DATA PANGAEA
  • 4
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    (Table 1) Lithology of DSDP Hole 24-237
    PANGAEA
    Details
    Publication Date: 2023-06-27
    Keywords: 24-237; AGE; Carbonates; Deep Sea Drilling Project; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Indian Ocean//PLATEAU; Leg24; Lithology/composition/facies; Sediment thickness
    Type: Dataset
    Format: text/tab-separated-values, 105 data points
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    DATA PANGAEA
  • 5
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    Seismic stratigraphy of Cretaceous eastern Central Atlantic Ocean: Basin evolution and palaeoceanographic implications (2018)
    Elsevier
    In:  Earth and Planetary Science Letters, 499 . pp. 107-121.
    Details
    Publication Date: 2021-02-08
    Description: Highlights • Morphology and evolution of a Cretaceous contourite drift in the eastern Central Atlantic oceanic basin. • Backstripping of the regional cross section reveals the water-depth range at which the observed sedimentary features occur. • Cretaceous geological interval and oceanic model mirrors the stratification of the Modern Ocean and the morphology of its seafloor. Abstract The evolution and resulting morphology of a Cretaceous contourite drift in the eastern Central Atlantic oceanic basin is investigated in unprecedented detail using seismic imaging and age-calibrated cross-margin sections. The margin, from the shelf, slope to deep-water and abyssal plain is constructed by a succession of erosive and depositional mounded structures that relate to bottom-water currents and sediment winnowing. The regional mapping of these drifts, sediment waves and gravitational sedimentary systems allows us to test the Upper Cretaceous paleocirculation model. Combined with flexural backstripping of the regional cross section, it reveals the water-depth range at which the observed sedimentary features occur. A possible late Albian to Turonian contourite drift system is observed from Guinea to Mauritania. The development of a shallow to deep oceanic circulation system is a key element in the rock record, with implications for the palaeoceanography and layering of the Cretaceous ocean. The Cretaceous geological interval and oceanic model mirrors the stratification of the modern ocean and the morphology of its seafloor from offshore Morocco to Guinea.
    Type: Article , PeerReviewed
    Format: text
    DOI: 10.1016/j.epsl.2018.07.023
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    OceanRep: Article in a Scientific Journal - peer-reviewed
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