Abstract The Central Asian Orogenic Belt (CAOB, also known as the Altaid Tectonic
Collage), one of the largest and long-lived accretionary orogens in the world, developed …

The CHONS elements that constitute the outgassed atmosphere and exosphere have likely
been delivered by chondritic materials to the Earth during planetary accretion and …

A global selection of 56 mid-ocean ridge basalt (MORB) glasses were analysed for Li and B
abundances and isotopic compositions. Analytical accuracy and precision of analyses …

The Late Carboniferous to Permian is a critical period for final amalgamation of the Central
Asian Orogenic Belt (CAOB). Gabbroic and granitic intrusions formed in this period at …

The concentration of carbon in primary mid‐ocean ridge basalts (MORBs), and the
associated fluxes of CO2 outgassed at ocean ridges, is examined through new data …

The Kangurtag belt in the Eastern Tianshan, connecting the Dananhu Arc with the Central
Tianshan Arc, contains diagnostic rocks of accretionary origin, and thus provides key …

In order to better characterise mantle CO2/Nb-variability, we obtained and compiled major
and trace elements, content and isotope composition of both CO2 and water on two series of …

In order to constrain better the distribution, age, geochemistry and origin of widespread
Cenozoic intraplate volcanism on Zealandia, the New Zealand micro-continent, we report …

The cycling of material from Earth's surface environment into its interior can couple mantle
oxidation state to the evolution of the oceans and atmosphere. A major uncertainty in this …

Mafic magmas generated in extensional tectonic settings preserve important information
about the nature of their mantle sources, interactions between crust and mantle, and the …