Nadir Halim

发表

Tectonic evolution of the Tancheng‐Lujiang (Tan‐Lu) fault via Middle Triassic to Early Cenozoic paleomagnetic data

Yan Chen, Xixi Zhao, Vincent Courtillot, 1999 .

Resolving the problem of shallow magnetizations of Tertiary age in Asia: insights from paleomagnetic data from the Qiangtang, Kunlun, and Qaidam blocks (Tibet, China), and a new hypothesis

Yan Chen, V. Courtillot, J. Cogné, 1999 .

Late Jurassic-Early Cretaceous closure of the Mongol-Okhotsk Ocean demonstrated by new Mesozoic palaeomagnetic results from the Trans-Baïkal area (SE Siberia)

Vadim A. Kravchinsky, J. Cogné, Fatim Hankard, 2005 .

A palaeomagnetic study from the Mongol–Okhotsk region: rotated Early Cretaceous volcanics and remagnetized Mesozoic sediments

A. A. Sorokin, S. Gilder, Yan Chen, 1998 .

New paleomagnetic constraints on central Asian kinematics: Displacement along the Altyn Tagh fault and rotation of the Qaidam Basin

S. Gilder, Yan Chen, V. Courtillot, 2002 .

Paleomagnetic study of Upper Jurassic rocks from the Sichuan basin: tectonic aspects for the collision between the Yangtze Block and the North China Block

Y. Otofuji, Yuyan Liu, Nadir Halim, 2001 .

Late Cretaceous palaeomagnetic results from Sikhote Alin, far eastern Russia: tectonic implications for the eastern margin of the Mongolia Block

R. Enami, H. Zaman, V. G. Sakhno, 2003 .

Palaeomagnetic evidence for southward displacement of the Chuan Dian fragment of the Yangtze Block

H. Zaman, Y. Otofuji, Yuyan Liu, 2004 .

New Cretaceous and Early Tertiary paleomagnetic results from Xining‐Lanzhou basin, Kunlun and Qiangtang blocks, China: Implications on the geodynamic evolution of Asia

S. Gilder, J. Marcoux, J. Besse, 1998 .

New paleomagnetic constraints on the extrusion of Indochina: Late Cretaceous results from the Song Da terrane, northern Vietnam

S. Hada, Y. Otofuji, Nadir Halim, 2005 .

New Mesozoic and Cenozoic data help constrain the age of motion on the Altyn Tagh fault and rotation of the Qaidam basin.

S. Gilder, Yan Chen, V. Courtillot, 2002 .