The vast eastern-Tethyan oceanic domain that throughout the Mesozoic extended between
Gondwana and Eurasia was a puzzle of larger and smaller microcontinents separated by …

Abstract The Neo-Tethys Ocean was an eastward-ga** triangular oceanic embayment
between Laurasia to the north and Gondwana to the south. The Neo-Tethys Ocean was …

The detrital zircon has been most widely used in sediment provenance studies and basin
analysis over the past 20 years. With the accumulation of a bounty of detrital zircon ages …

Abstract Although the Cenozoic Indo-Asian collision is largely responsible for the formation
of the Tibetan plateau, the role of pre-Cenozoic structures in controlling the timing and …

The tectono-magmatic evolution of the Bangong-Nujiang Tethyan Ocean (BNO) plays a
crucial role in understanding the Tibetan Plateau accretion before the Cenozoic India-Asia …

Abstract To constrain the Lhasa-Qiangtang collisional age, a combined paleomagnetic and
geochronologic investigation has been performed on the Risong Formation redbeds and …

It is generally accepted that the subduction polarity reversal (SPR) results from the strong
collision of two plates. Yet, the SPR of the Solomon Back‐arc Basin is started in the “soft …

The southern Myanmar tin ore district is an important part of the well-known Southeast Asia
tin belt (SATB), and hosts numerous economically important primary tin-tungsten ore …

Abstract The Bangong–Nujiang Ocean played an important role in the formation of the
Tibetan Plateau prior to the Cenozoic India–Eurasia collision. However, there are still …

In order to study the rotations of crustal material along the boundary faults in the
southeastern Tibetan Plateau, and to better understand the tectonic evolution of this region …