Supplementary Tables S1 to S6.xlsx

Name: Supplementary Tables S1 to S6.xlsx
Creator: 朱, 传威
Published: 2024-02-27T00:00:00+08:00

Figshare2024-02-27 更新2026-04-08 收录

岩石地球化学

洋中脊地质调查

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Major and trace elements of MORB samples from East Pacific Rise and Southwest Indian Ridge

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朱, 传威

创建时间：

2024-02-27

Table S1-S7 in the manuscript titled "Large-scale Cretaceous adakitic magmatism induced by water-fluxed melting of continental crust during the North China Craton destruction".

岩石地球化学

同位素年代学

The whole-rock geochemistry and zircon Hf-O isotopic data, zircon U-Pb dating, major and trace elements chosen for thermodynamic simulations and trace element characteristics modelling in the study. T

Figshare2023-08-30 更新50

EF value of trace elements of dark shale samples from Member1 of Upper Carboniferous Keluke Formation in Huaitoutela area, eastern NMQB.

岩石地球化学

微量元素富集因子

EF value of trace elements of dark shale samples from Member1 of Upper Carboniferous Keluke Formation in Huaitoutela area, eastern NMQB.

NIAID Data Ecosystem30

Tab.1: Representative bulk-rock and trace element chemistry

岩石地球化学

变质岩分析

High-pressure/low-temperature metabasites occupy a definite geological position within the structure of the Polar Urals and have a very important bearing on the understanding of...

B2FIND20

Geochemistry and tectonic significance of the Fannuj-Maskutan SSZ-type ophiolite (Inner Makran, SE Iran)

SSZ型蛇绿岩

岩石地球化学

The nature and geodynamic setting of Inner Makran ophiolites (SE Iran) are controversial and are the focus of a growing debate. The Fannuj-Maskutan ophiolite complex (central Inner Makran) is made up

NIAID Data Ecosystem30

Petrology of Late Jurassic allochthonous ultramafic lamprophyres within the Batain Nappes, Northeastern Oman

岩石地球化学

煌斑岩成因

Late Jurassic ultramafic lamprophyre (UML) sills and dikes occur as 3 km-long intrusions within the allochthonous Whara Formation of the Batain nappes, eastern Oman. The sills and dikes comprise macro

Taylor & Francis Group2016-01-20 更新30

Supplementary Tables S1 to S6.xlsx

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