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• W1986045856 endingPage "641" @default.
• W1986045856 startingPage "625" @default.
• W1986045856 abstract "Abstract To further constrain the India–Asia collisional process, a combined paleomagnetic and geochronologic study has been carried out on the Upper Cretaceous Jingzhushan Formation redbeds and the Lower Cretaceous Dianzhong Formation volcanic rocks dated at ~ 121–117 Ma from the Cuoqin area in the central Lhasa terrane. Stepwise thermal demagnetization successfully isolated reliable characteristic remanent magnetization (ChRM) directions that include dual polarity and pass positive fold tests at 95% and 99% confidence levels, indicating prefolding primary magnetizations. The tilt-corrected site-mean direction for 33 redbed sites is D = 316.8°, I = 30.2° with α 95  = 5.4°, corresponding to a paleopole at 49.0°N, 344.3°E with A 95  = 5.3°, and the other for 12 volcanic sites is D = 350.5°, I = 25.5° with α 95  = 7.7°, corresponding to a paleopole at 70.5°N, 292.9°E with A 95  = 7.4°. Our new paleomagnetic results, together with reliable Cretaceous paleomagnetic data obtained from the Lhasa terrane, demonstrate that the southern margin of Asia was located at ~ 15.1°N during the Cretaceous. Comparison with the apparent polar wander paths (APWP) of India and the Cretaceous–Paleocene paleopoles of the Himalayan terrane suggests that the India–Asia collision was likely a complex process, which consists of the collision of the Lhasa and Himalayan terranes at 54.0 ± 2.1 Ma, the longtime subduction of an intra-oceanic basin between the Himalayan terrane and the Indian craton from ~ 54.0 to ~ 40.4 Ma, and the collision of the Himalayan terrane and the Indian craton at 40.4 ± 4.1 Ma. Comparing with the Late Cretaceous average pole of the East Asia APWP reveals that a latitudinal convergence of 780 ± 240 km has taken place between the Lhasa terrane and East Asia (the Hexi corridor) since the India–Asia collision; the amount of latitudinal shortening deduced from paleomagnetic data is very consistent with the 600–1000 km accommodated by the Cenozoic fold and thrust belts between the Lhasa terrane and Hexi corridor." @default.
• W1986045856 created "2016-06-24" @default.
• W1986045856 creator A5019251037 @default.
• W1986045856 creator A5027024676 @default.
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• W1986045856 creator A5085231444 @default.
• W1986045856 date "2015-09-01" @default.
• W1986045856 modified "2023-10-10" @default.
• W1986045856 title "New insights into the India–Asia collision process from Cretaceous paleomagnetic and geochronologic results in the Lhasa terrane" @default.
• W1986045856 cites W1597063492 @default.
• W1986045856 cites W1607805073 @default.
• W1986045856 cites W1649557696 @default.
• W1986045856 cites W1658256170 @default.
• W1986045856 cites W1769330608 @default.
• W1986045856 cites W1830210718 @default.
• W1986045856 cites W1839380302 @default.
• W1986045856 cites W1959048442 @default.
• W1986045856 cites W1968185136 @default.
• W1986045856 cites W1968485739 @default.
• W1986045856 cites W1969447332 @default.
• W1986045856 cites W1970546147 @default.
• W1986045856 cites W1973776603 @default.
• W1986045856 cites W1975969841 @default.
• W1986045856 cites W1976467450 @default.
• W1986045856 cites W1976963145 @default.
• W1986045856 cites W1979228363 @default.
• W1986045856 cites W1980364678 @default.
• W1986045856 cites W1981295689 @default.
• W1986045856 cites W1982940988 @default.
• W1986045856 cites W1985616609 @default.
• W1986045856 cites W1987562178 @default.
• W1986045856 cites W1988550561 @default.
• W1986045856 cites W1990045396 @default.
• W1986045856 cites W1990713790 @default.
• W1986045856 cites W1993331363 @default.
• W1986045856 cites W1997698506 @default.
• W1986045856 cites W2002325302 @default.
• W1986045856 cites W2004780129 @default.
• W1986045856 cites W2006723695 @default.
• W1986045856 cites W2008461587 @default.
• W1986045856 cites W2011834231 @default.
• W1986045856 cites W2014678427 @default.
• W1986045856 cites W2016342693 @default.
• W1986045856 cites W2016760315 @default.
• W1986045856 cites W2017071350 @default.
• W1986045856 cites W2019038128 @default.
• W1986045856 cites W2019748000 @default.
• W1986045856 cites W2020518963 @default.
• W1986045856 cites W2020973699 @default.
• W1986045856 cites W2021451790 @default.
• W1986045856 cites W2022859730 @default.
• W1986045856 cites W2023828447 @default.
• W1986045856 cites W2023910005 @default.
• W1986045856 cites W2029746347 @default.
• W1986045856 cites W2031516303 @default.
• W1986045856 cites W2032822582 @default.
• W1986045856 cites W2032839284 @default.
• W1986045856 cites W2033011597 @default.
• W1986045856 cites W2034397592 @default.
• W1986045856 cites W2041342642 @default.
• W1986045856 cites W2041774199 @default.
• W1986045856 cites W2043020354 @default.
• W1986045856 cites W2053460385 @default.
• W1986045856 cites W2055794724 @default.
• W1986045856 cites W2056886054 @default.
• W1986045856 cites W2061544674 @default.
• W1986045856 cites W2065105994 @default.
• W1986045856 cites W2069504073 @default.
• W1986045856 cites W2069716890 @default.
• W1986045856 cites W2084045184 @default.
• W1986045856 cites W2088749005 @default.
• W1986045856 cites W2089579858 @default.
• W1986045856 cites W2093873338 @default.
• W1986045856 cites W2095800081 @default.
• W1986045856 cites W2095892702 @default.
• W1986045856 cites W2096622871 @default.
• W1986045856 cites W2096716153 @default.
• W1986045856 cites W2112908975 @default.
• W1986045856 cites W2115518283 @default.
• W1986045856 cites W2116527388 @default.
• W1986045856 cites W2118204502 @default.
• W1986045856 cites W2118515467 @default.
• W1986045856 cites W2123588493 @default.
• W1986045856 cites W2123779550 @default.
• W1986045856 cites W2138644850 @default.
• W1986045856 cites W2140093647 @default.
• W1986045856 cites W2142145377 @default.
• W1986045856 cites W2148458203 @default.
• W1986045856 cites W2149951012 @default.
• W1986045856 cites W2150230180 @default.
• W1986045856 cites W2152546160 @default.
• W1986045856 cites W2154296177 @default.
• W1986045856 cites W2155879688 @default.

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