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- W2361003578 abstract "A total of 3791 systematic oriented paleomagnetic samples were collected from the Ordovician -Paleogene nearly consecutive sedimentary rocks on the northern slope of the Himalayas, southern Tibet, of which 2920 samples were analyzed and took part in the statistics. New magnetostratigraphic data of the series-rank were obtained and the Ordovician-Paleogene paleomagnetic apparent polar wander path and paleo-latitude curve of the Himalayan block were drawn. The paleomagnetic records suggest that the Himalayan block rotated several times during its northward drifting and that the final ～28° clockwise rotation took place in the Eocene, which is probably related to the formation of the western tectonic syntax. South-directed inversions of 2° and 3.8° in latitude were recorded during the Late Triassic and Late Jurassic, which is likely to be related to the back-arc spreading of the Yarlung Zangbo Neo-Tethys Ocean. Based on the estimation of the paleo-latitude data, the Middle Cretaceous Yarlung Zangbo Neo-Tethys oceanic basin was at least 2200 km wide, and there was a crustal shortening amount of at least 1000 km between the Indian plate, Himalayan fold-thrust belt and Lhasa block resulting from the Himalayan continent-continent collisional orogeny since the Eocene." @default.
- W2361003578 created "2016-06-24" @default.
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- W2361003578 date "2006-01-01" @default.
- W2361003578 modified "2023-09-28" @default.
- W2361003578 title "New Ordovician-Paleogene tectonomagnetic data from the northern slope of the Himalayas." @default.
- W2361003578 hasPublicationYear "2006" @default.
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