Sediments of the west part of the Valjevo-Mionica basin (Serbia) were examined both geochemically and mineralogically to explain, on the basis of their sediment
Serpentinites from the inside cer high (6°38.5’S/ 68°19.34’E) from the North Central Indian Ridge (NCIR) are comprised mainly of high Mg-rich lizardite and
The Ordos basin was developed from Mid-Late Triassic to Early Cretaceous, and then entered into its later reformation period since the Late Cretaceous. Its main
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