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Sr-Nd isotopic compositions for the Woniusi rock associations
Note: 87Rb/86Sr and 147Sm/144Nd are calculated using whole-rock Rb, Sr, Sm and Nd values in Table S4. Initial isotopic ratios are corrected to measured age. (87Sr/86Sr)i =... -
Major and trace elements of the Woniusi rock associations
a FeOT, total iron as FeO, FeOT=FeO+0.9 *Fe2O3. b LOI, loss on ignition. c Mg# = 100 × Mg/(Mg + Fetotal) in atomic ratio. -
Zircon Lu-Hf isotopic data for zircons of the Late Paleozoic mafic rocks in t...
Note: The present 176Hf/177Hf and 176Lu/177Hf ratios of chondrite and depleted mantle are 0.282772 and 0.0332, and 0.28325 and 0.0384, respectively, Blichert-Toft and Albarède... -
Geochronological data of the Woniusi rock associations
This dataset has no description
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Zircon U-Pb isotopic data for the Woniusi rock associations
This dataset has no description
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Tholeiitic magmatic record on an extensional passive continental margin from ...
Basaltic samples of the Woniusi rock assocation were collected from the northern, middle, and southern parts of the Baoshan block. Basaltic samples were selected for whole-rock... -
Morphotectonic Evolution of Passive Margins undergoing Active Surface Process...
Extension of the continental lithosphere can lead to the formation of rifted margins with contrasting tectonic and geomorphologic characteristics. Many of these characteristics... -
Melt volume at Atlantic volcanic rifted margins controlled by depth-dependent...
Breakup volcanism along rifted passive margins is highly variable in time and space. The factors controlling magmatic activity during continental rifting and breakup are not...
