Continental crustal growth processes recorded in the Gangdese Batholith, southern Tibet
The continental crust in the overriding plate of the India-Asia collision zone in southern Tibet
is characterized by an overthickened layer of felsic composition with an underlying granulite …
is characterized by an overthickened layer of felsic composition with an underlying granulite …
Towards a universal model for orogenic gold systems: A perspective based on Chinese examples with geodynamic, temporal, and deposit-scale structural and …
Although the term orogenic gold has become widely accepted over the past 20 years for
disseminated-to lode-style gold deposits that formed in a variety of tectonic environments …
disseminated-to lode-style gold deposits that formed in a variety of tectonic environments …
[PDF][PDF] Mesozoic–Cenozoic geological evolution of the Himalayan-Tibetan orogen and working tectonic hypotheses
P Kapp, PG DeCelles - American Journal of Science, 2019 - ajsonline.org
The Himalayan-Tibetan orogen culminated during the Cenozoic India--Asia collision, but its
geological framework and initial growth were fundamentally the result of multiple, previous …
geological framework and initial growth were fundamentally the result of multiple, previous …
Tibetan ore deposits: A conjunction of accretionary orogeny and continental collision
This paper reviews the spatial-temporal distribution, geological and geochemical features,
and geophysical context of diverse types of Cenozoic ore deposits formed during India …
and geophysical context of diverse types of Cenozoic ore deposits formed during India …
Origin of postcollisional magmas and formation of porphyry Cu deposits in southern Tibet
The recent discovery of large porphyry copper deposits (PCDs) associated with Miocene (22–
12 Ma) granitoid magmas in the eastern section of the Paleocene-Eocene Gangdese …
12 Ma) granitoid magmas in the eastern section of the Paleocene-Eocene Gangdese …
Raising the Gangdese mountains in southern Tibet
The surface uplift of mountain belts is in large part controlled by the effects of crustal
thickening and mantle dynamic processes (eg, lithospheric delamination or slab breakoff) …
thickening and mantle dynamic processes (eg, lithospheric delamination or slab breakoff) …
Processes of initial collision and suturing between India and Asia
The initial collision between Indian and Asian continents marked the starting point for
transformation of land-sea thermal contrast, uplift of the Tibet-Himalaya orogen, and climate …
transformation of land-sea thermal contrast, uplift of the Tibet-Himalaya orogen, and climate …
[HTML][HTML] Geological, geophysical and plate kinematic constraints for models of the India-Asia collision and the post-Triassic central Tethys oceans
In this study, we integrate bedrock datasets, observations of subducted slabs in the mantle,
and plate kinematic constraints to constrain models for the India-Asia collision and the …
and plate kinematic constraints to constrain models for the India-Asia collision and the …
Insight into zircon REE oxy-barometers: A lattice strain model perspective
Zircon rare earth element (REE) oxy-barometers have been widely used to calculate magma
oxygen fugacity. However, sometimes confusing results are obtained, such as extremely …
oxygen fugacity. However, sometimes confusing results are obtained, such as extremely …
The Himalayan collisional orogeny: A metamorphic perspective
This paper introduces how crustal thickening controls the growth of the Himalaya by
summarizing the P‐T‐t evolution of the Himalayan metamorphic core. The Himalayan …
summarizing the P‐T‐t evolution of the Himalayan metamorphic core. The Himalayan …