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Boron/Calcium and Magnesium/Calcium ratios measured on Cibicidoides wuellerst...
This dataset has no description
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Boron/Calcium and Magnesium/Calcium ratios measured on Cibicidoides mundulus ...
This dataset has no description
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Boron/Calcium ratio measured on Cibicidoides cf. wuellerstorfi and Cibicidoid...
This dataset has no description
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Boron/Calcium ratio measured on Cibicidoides wuellerstorfi and Uvigerina spp....
This dataset has no description
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Boron/Calcium ratio measured on Cibicidoides cf. wuellerstorfi of sediment co...
This dataset has no description
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The inorganic carbon system measured and calculated on Cibicidoides mundulus ...
Reconstruction equation: B/Ca = 0.80(D[CO32-]) + 114.5 (R2=0.79) -
The inorganic carbon system measured and calculated on Cibicidoides cf. wuell...
Reconstruction equation: B/Ca = 2.27(D[CO32-]) + 152.5 (R2= 0.76) -
The inorganic carbon system measured and calculated on Cibicidoides cf. wuell...
Reconstruction equation: B/Ca = 2.27(D[CO32-]) + 152.5 (R2= 0.76) -
The inorganic carbon system measured and calculated on Cibicidoides cf. wuell...
Reconstruction equation: B/Ca = 2.27(D[CO32-]) + 152.5 (R2= 0.76) -
The inorganic carbon system measured and calculated on Cibicidoides wuellerst...
Reconstruction equation: B/Ca = 1.39(D[CO32-]) + 175.5 (R**2 = 0.87) -
The inorganic carbon system measured and calculated on Cibicidoides wuellerst...
Reconstruction equation: B/Ca = 1.39(D[CO32-]) + 175.5 (R2= 0.87) -
Summary of phase compositions of experimental silicate melt, un-normalised an...
The solubility of Re and Au in haplobasaltic melt has been investigated at 1673–2573 K, 0.1 MPa–2 GPa and IW-1 to +2.5, in both carbon-saturated and carbon-free systems. Results... -
U-Pb, trace element, and Hf isotope analysis for Macquarie Island detrital zi...
Oceanic zircon trace element and Hf-isotope geochemistry offers a means to assess the magmatic evolution of a dying spreading ridge and provides an independent evaluation of the... -
Table A1 LA-ICP-MS zircon U-Pb data of Laoniushan granitoids
The NWW-striking Qinling Orogen formed in the Triassic by collision between the North China and Yangtze Cratons. Triassic granitoid intrusions, mostly middle- to high-K,...
