Add to ORKGWe are investigating peridotite alteration in the mantle section of the Samail ophiolite in Oman. Understanding the natural system provides insights into design of enhanced, in situ mineral carbonation for CO_2 storage, and ‘negative emissions’ via enhanced CO_2 capture from surface waters
金沢大学理工研究域地球社会基盤学系Completely carbonated peridotites represent a window to study reactions of carbon-r...
The radiocarbon isotope data of aragonite, calcite, and dolomite veins and whole-rock total inorgani...
Earth’s long-term cycling of carbon is regulated from mid-ocean ridges to convergent margins by mass...
A large part of the hydrated oceanic lithosphere consists of serpentinites exposed in ophiolites. Se...
Carbon dioxide capture and storage will be necessary to mitigate the effects of global climate chang...
The low-temperature alteration of peridotite in ophiolites produces two types of fluids, Mg-HCO3- ri...
International audienceThe Wadi Dima area (Oman Ophiolite) exposes partially altered to highly serpen...
International audienceCompletely carbonated peridotites represent a window to study reactions of car...
Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the M...
Fully carbonated peridotite, known as listvenite, is well exposed along the basal thrust of the Oman...
Near-surface reaction of CO2-bearing fluids with silicate minerals in peridotite and basalt forms so...
In situ sequestration of CO2 in mantle peridotites has been proposed as a method to alleviate the am...
The clumped and oxygen isotopes of dolomite from ultramafic rocks recovered during ICDP Expedition 5...
The formation of carbonate minerals during alteration of ultramafic rocks represents a geological an...
AbstractMineral carbonation is a process whereby CO2 reacts with ultramafic rocks to form carbonate ...
金沢大学理工研究域地球社会基盤学系Completely carbonated peridotites represent a window to study reactions of carbon-r...
The radiocarbon isotope data of aragonite, calcite, and dolomite veins and whole-rock total inorgani...
Earth’s long-term cycling of carbon is regulated from mid-ocean ridges to convergent margins by mass...
A large part of the hydrated oceanic lithosphere consists of serpentinites exposed in ophiolites. Se...
Carbon dioxide capture and storage will be necessary to mitigate the effects of global climate chang...
The low-temperature alteration of peridotite in ophiolites produces two types of fluids, Mg-HCO3- ri...
International audienceThe Wadi Dima area (Oman Ophiolite) exposes partially altered to highly serpen...
International audienceCompletely carbonated peridotites represent a window to study reactions of car...
Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the M...
Fully carbonated peridotite, known as listvenite, is well exposed along the basal thrust of the Oman...
Near-surface reaction of CO2-bearing fluids with silicate minerals in peridotite and basalt forms so...
In situ sequestration of CO2 in mantle peridotites has been proposed as a method to alleviate the am...
The clumped and oxygen isotopes of dolomite from ultramafic rocks recovered during ICDP Expedition 5...
The formation of carbonate minerals during alteration of ultramafic rocks represents a geological an...
AbstractMineral carbonation is a process whereby CO2 reacts with ultramafic rocks to form carbonate ...
金沢大学理工研究域地球社会基盤学系Completely carbonated peridotites represent a window to study reactions of carbon-r...
The radiocarbon isotope data of aragonite, calcite, and dolomite veins and whole-rock total inorgani...
Earth’s long-term cycling of carbon is regulated from mid-ocean ridges to convergent margins by mass...