The Panjal Traps

    研究成果: 書貢獻/報告類型篇章

    15 引文 斯高帕斯(Scopus)

    摘要

    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 that range from continental tholeiite to ocean-floor basalt but it is clear that crustal contamination has played a role in their genesis. The basalts that show limited evidence for contamination have Sr-Nd isotopes (87Sr/86Sri = 0.7043-0.7073; εNd(t) = 0 ± 1) similar to a chondritic (subcontinental lithospheric mantle) source, whereas the remaining basaltic rocks have a wide range of Nd (εNd(t) = -6.1 to +4.3) and Sr (87Sr/86Sri = 0.7051-0.7185) isotopic values. The primary melt composition of the low-Ti Panjal Traps is picritic with mantle potential temperatures (TP = 1400°C to 1450°C) similar to ambient mantle. The silicic volcanic rocks were derived by partial melting of the crust, whereas the andesitic rocks were derived by mingling between crustal and mantle melts. The Panjal Traps initially erupted within a continental rift setting. The rift eventually transitioned into a nascent ocean basin that led to seafloor spreading and the formation of the Neotethys Ocean and the ribbonlike continent Cimmeria.

    原文英語
    主出版物標題Geological Society Special Publication
    發行者Geological Society of London
    頁面59-86
    頁數28
    版本1
    DOIs
    出版狀態已發佈 - 2018 一月 1

    出版系列

    名字Geological Society Special Publication
    號碼1
    463
    ISSN(列印)0305-8719

    ASJC Scopus subject areas

    • 水科學與技術
    • 海洋工程
    • 地質學

    指紋

    深入研究「The Panjal Traps」主題。共同形成了獨特的指紋。

    引用此