In order to better constrain the evolution of the Tethyan orogenic system, we conducted an
integrated investigation involving U-Pb dating of igneous and detrital zircon, geochemical …

摘要印度与亚洲的碰撞及前期的地体拼合产生了世界上规模最大的青藏高原碰撞造山带,
并进面导致了高原的形成. 但关于该造山带的形成产化过程与高原隆升的关系 …

The geodynamic evolution of the Tibetan Plateau remains highly debated. Any model of its
evolution must explain the plateau's growth as constrained by palaeo-altitude studies, the …

The composition of the deep crust is a key to understanding the formation of the low-velocity
zone in the middle to lower crust of the Tibetan Plateau. The Suyingdi rhyolites exposed in …

It is generally believed that Cenozoic potassic and ultrapotassic volcanic rocks of the
Tibetan Plateau were generated by partial melting of enriched mantle. This paper reports …

Shear-wave splitting provides insight into geodynamic processes such as lithospheric
deformation and upper mantle flow. This study presents shear wave splitting parameters …

Chah-Shaljami porphyritic granitoids belong to the Lut Block volcanic–plutonic belt of central
eastern Iran. These intrusive rocks are mostly quartz monzonites, granodiorites and diorites …

Abstract The Dehsalm Cu–Mo-bearing porphyritic granitoids belong to the Lut Block
volcanic–plutonic belt (central eastern Iran). These rocks range in composition from gabbro …

The time and mechanism of crustal thickening and initial surface uplift of the Tibetan Plateau
remain highly controversial. Here we report on zircon U‐Pb age, and mineral, element, and …

A zircon U–Pb age of adakitic rocks from Jiaodong, the Shandong Province, indicates that
the volcanic rocks erupted at 123.6±0.8 Ma. The volcanic rocks are composed only of …