In this study,we determined the granite ages in the middle to east Gangdese batholith. Zircon ages from these granites are 57.6–68.7 Ma,indicating that intrusions were formed in the Late Cretaceous to early Paleocene. The large-ion lithophile elements are highly enriched,whereas some high-field-stre...2441-4668
Abstract The Gangdese belt of the southern Lhasa terrane (southern Tibet) records a Chileantype accr...
The Gangdese magmatic belt of southern Tibet is an ideal place to study Neo-Tethyan subduction, cont...
The petrogenesis and geodynamic implications of the Cenozoic adakites in southern Tibet remain topic...
In this study, we determined the granite ages in the middle to east Gangdese batholith. Zircon ages ...
The Gangdese batholith emplaced from the Cretaceous to Eocene in southern Tibet has been widely rega...
Voluminous peraluminous leucogranites are common in large-scale orogenic belts and are crucial in ga...
The Paleocene-Eocene ore deposits in the Gangdese Metallogenic Belt, Tibet, are thought to have been...
Geochronological data from the Golmud--Lhasa section across the Tibetan Plateau indicate progressive...
The Gangdese belt in southern Tibet forms the eastern section of the Trans- Himalayan magmatic belt....
The major and trace-element geochemistry, Sr–Nd bulk-rock isotopes, U–Pb zircon chronology and Lu–Hf...
The Gangdese belt, Tibet, records the opening and closure of the Neo-Tethyan ocean and the resultant...
<p>The Tibetan Plateau is a composite orogenic belt that has experienced prolonged subduction, obduc...
At more than 500 km in length, the mainly Jurassic–Early Eocene Gangdese batholith is one of the mos...
The Nyingchi complex, forming the eastern segment of the Gangdese magmatic arc, occurs within the so...
There continues to be debate regarding the timing of the collision between the Indian and Eurasian p...
Abstract The Gangdese belt of the southern Lhasa terrane (southern Tibet) records a Chileantype accr...
The Gangdese magmatic belt of southern Tibet is an ideal place to study Neo-Tethyan subduction, cont...
The petrogenesis and geodynamic implications of the Cenozoic adakites in southern Tibet remain topic...
In this study, we determined the granite ages in the middle to east Gangdese batholith. Zircon ages ...
The Gangdese batholith emplaced from the Cretaceous to Eocene in southern Tibet has been widely rega...
Voluminous peraluminous leucogranites are common in large-scale orogenic belts and are crucial in ga...
The Paleocene-Eocene ore deposits in the Gangdese Metallogenic Belt, Tibet, are thought to have been...
Geochronological data from the Golmud--Lhasa section across the Tibetan Plateau indicate progressive...
The Gangdese belt in southern Tibet forms the eastern section of the Trans- Himalayan magmatic belt....
The major and trace-element geochemistry, Sr–Nd bulk-rock isotopes, U–Pb zircon chronology and Lu–Hf...
The Gangdese belt, Tibet, records the opening and closure of the Neo-Tethyan ocean and the resultant...
<p>The Tibetan Plateau is a composite orogenic belt that has experienced prolonged subduction, obduc...
At more than 500 km in length, the mainly Jurassic–Early Eocene Gangdese batholith is one of the mos...
The Nyingchi complex, forming the eastern segment of the Gangdese magmatic arc, occurs within the so...
There continues to be debate regarding the timing of the collision between the Indian and Eurasian p...
Abstract The Gangdese belt of the southern Lhasa terrane (southern Tibet) records a Chileantype accr...
The Gangdese magmatic belt of southern Tibet is an ideal place to study Neo-Tethyan subduction, cont...
The petrogenesis and geodynamic implications of the Cenozoic adakites in southern Tibet remain topic...