Paleomagnetic samples were collected from four localities located in the southern rim of the Tarim basin. The samples were taken from volcanic rocks erupted between Jurassic and Quaternary. Detailed analysis of all sa...Paleomagnetic samples were collected from four localities located in the southern rim of the Tarim basin. The samples were taken from volcanic rocks erupted between Jurassic and Quaternary. Detailed analysis of all samples has been carried out with progressive thermal demagnetization. A characteristic remanence (ChRM) with higher unblocking temperature has been isolated from all samples. The pole position from the middle Jurassic is at 52.5°N, 187 9°E ( dp =3.7°, dm =6.5°); the directions of the ChRM of Cretaceous correspond to a paleopole at 69.7°N, 211.6°E ( dp =9.8°, dm =15.9°); the Quaternary pole from the Pulu site is at 79.9°N, 183.1°E ( dp =1.6°, dm = 2.4°). On the basis of these new paleomagnetic data, tectonic evolution of Tarim block is presented.展开更多
文摘Paleomagnetic samples were collected from four localities located in the southern rim of the Tarim basin. The samples were taken from volcanic rocks erupted between Jurassic and Quaternary. Detailed analysis of all samples has been carried out with progressive thermal demagnetization. A characteristic remanence (ChRM) with higher unblocking temperature has been isolated from all samples. The pole position from the middle Jurassic is at 52.5°N, 187 9°E ( dp =3.7°, dm =6.5°); the directions of the ChRM of Cretaceous correspond to a paleopole at 69.7°N, 211.6°E ( dp =9.8°, dm =15.9°); the Quaternary pole from the Pulu site is at 79.9°N, 183.1°E ( dp =1.6°, dm = 2.4°). On the basis of these new paleomagnetic data, tectonic evolution of Tarim block is presented.
