XRD patterns and isotope data of 26 dolomite samples of the Marion Plateau (Site 816 and Site 1196). XRD Measurements were done at the Natural History Museum London with an XPERT-PRO diffractometer system over the 2theta range of 20-98 (CuKalpha). The step used was 0.017 [°2theta] with an integration time of 150 s. The position of the sensitive detector was 2.12 [°2theta] and the divergent slit size was 0.0626[°]. Isotopes oxygen, carbon and clumped isotopes dat
This work focuses on an exceptionally complex natural laboratory, the Triassic Latemar isolated plat...
Carbonate was micro-sampled from representative listvenite and serpentinite core sections of Hole BT...
Dolomite petrography and O-C-Sr isotope geochemistry (including Tables S1 and S2 and Figures S1A–S1C...
The formation of low-temperature dolomite (CaMg(CO3)2) continues to be enigmatic. By using a newly d...
Much debate exists on the extent to which early dolomites recrystallize and preserve the signature o...
Dolomitization is a common reaction in carbonate hydrocarbon reservoirs. The volume of hydrocarbons ...
Dolomite is a very common carbonate mineral in ancient sediments, but is rarely found in modern envi...
Dolomite clumped isotope compositions are indispensable for determining the temperatures and fluid s...
The temperature of formation of replacement dolomite and δ^(18)O(H_(2)O) of dolomitizing fluid in th...
WOS:000393125500003International audienceWidespread application of the novel clumped isotope paleoth...
Widespread application of the novel clumped isotope paleothermometer (Δ47) using dolomite samples fr...
A small-scale analytical technique for carbon and oxygen isotopic analyses of dolomite, siderite and...
This supplementary dataset contains raw XRD and isotopic data used to generate figure in the article...
The origin of Quaternary dolomites in continental environments (e.g. karst and lakes) is barely cons...
The main goal of our research on dolomites has been to better understand the composition of the flui...
This work focuses on an exceptionally complex natural laboratory, the Triassic Latemar isolated plat...
Carbonate was micro-sampled from representative listvenite and serpentinite core sections of Hole BT...
Dolomite petrography and O-C-Sr isotope geochemistry (including Tables S1 and S2 and Figures S1A–S1C...
The formation of low-temperature dolomite (CaMg(CO3)2) continues to be enigmatic. By using a newly d...
Much debate exists on the extent to which early dolomites recrystallize and preserve the signature o...
Dolomitization is a common reaction in carbonate hydrocarbon reservoirs. The volume of hydrocarbons ...
Dolomite is a very common carbonate mineral in ancient sediments, but is rarely found in modern envi...
Dolomite clumped isotope compositions are indispensable for determining the temperatures and fluid s...
The temperature of formation of replacement dolomite and δ^(18)O(H_(2)O) of dolomitizing fluid in th...
WOS:000393125500003International audienceWidespread application of the novel clumped isotope paleoth...
Widespread application of the novel clumped isotope paleothermometer (Δ47) using dolomite samples fr...
A small-scale analytical technique for carbon and oxygen isotopic analyses of dolomite, siderite and...
This supplementary dataset contains raw XRD and isotopic data used to generate figure in the article...
The origin of Quaternary dolomites in continental environments (e.g. karst and lakes) is barely cons...
The main goal of our research on dolomites has been to better understand the composition of the flui...
This work focuses on an exceptionally complex natural laboratory, the Triassic Latemar isolated plat...
Carbonate was micro-sampled from representative listvenite and serpentinite core sections of Hole BT...
Dolomite petrography and O-C-Sr isotope geochemistry (including Tables S1 and S2 and Figures S1A–S1C...