Carbon occurs in mantle samples in several chemical, mineralogical and morphological
forms. It has been observed as CO2, CH4 and CO in fluid inclusions, as carbonate, graphite …

As an important part of the Mediterranean-Himalayas geothermal belt, southern Tibet and
western Yunnan are the regions of China where high-temperature hydrothermal systems are …

Large-scale helium accumulations are rarely reported in tectonically active continental
subduction zones. This study shows geochemical variations in helium and other volatiles (N …

In the Nyainqentanglha (NQTL) massif, southern Tibet, a late Cenozoic, SE dip**, normal
fault exhumed an oblique section of crust in its footwall. U‐Th‐Pb dating of zircon and …

The Karakoram fault (KKF) is the 1000km-long strike-slip fault separating the western
Himalaya from the Tibetan Plateau. From geologic and geodetic data, the KKF is argued …

Tibet is characterized by extremely high terrestrial heat flow and widely distributed
hydrothermal systems, among which many are discharging geothermal waters with …

The isotopic composition of helium emitted from geothermal springs in the southern Tibetan
plateau, reported as Rc/RA (Rc= air corrected sample 3He/4He, RA= air 3He/4He), ranges …

The lithospheric structure of the Tibetan Plateau plays a key role in explaining the
underlying plateau formation mechanism (s) and growth history. Although many studies …

Hot springs in the Marsyandi Valley, Nepal, vent CO2 sourced from metamorphic fluids that
mix with shallow groundwaters before degassing near the Earth's surface. The δ13C of …

Geothermal resources in China are distributed throughout the country, with hydrothermal
systems of high temperature in the Tibet Autonomous Region, Yunnan Province and Taiwan …