Tibetan Plateau uplift and global cooling have generally been thought to have caused the drying of the Asian inland, but how and when these factors drove the aridification is unknown. The Xining Basin at the NE Tibetan Plateau received continuous Eocene–Miocene fine-grained sediments, providing an excellent opportunity to address this question. Here we present detailed rock magnetic and dif…

Tahun Terbit

2005

Edisi

Ed.4

ISBN/ISSN

979-691-263-5

Deskripsi Fisik

xxvi, 542 p.: ill.; 26 cm.

No. Panggil

657.45 MES a