XHD-PSC-Supporting-Information-20191231.pdf

NIAID Data Ecosystem2026-03-11 收录

花岗岩成因

岩浆过程模拟

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https://figshare.com/articles/dataset/XHD-PSC-Supporting-Information-20191231_pdf/11479053 数据链接链接失效反馈

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The supporting information of recent submission (Rapid cooling and followed crystallization of ascending magma as an explanation for the origin of enclaves and host granitic rocks in South China Block)

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2020-04-08

Table_1_Early Jurassic Rare Metal Granitic Pluton of the Central Asian Orogenic Belt in North-Central Mongolia: Tungsten Mineralization, Geochronology, Petrogenesis and Tectonic Implications.XLSX

钨矿化

花岗岩成因

The Tukhum granitic pluton is a part of the Mesozoic composite Khentei batholith of north-central Mongolia, which belongs to the Central Asian Orogenic Belt. The shallow-seated pluton (∼900 km2) is ma

NIAID Data Ecosystem180

Evidence for hybridisation in the Tynong Province granitoids, Lachlan Fold Belt, eastern Australia

岩浆混合

花岗岩成因

The role of mafic–felsic magma mixing in the formation of granites is controversial. Field evidence in many granite plutons undoubtedly implies interaction of mafic (basaltic–intermediate) magma with

NIAID Data Ecosystem60

Petrogenesis and tectonic of the Urucum granitic suite, Rio Doce Valley (Minas Gerais - Brazil): an example of syn to late collisional peraluminous magmatism associated with high-angle transcurrent shear zone

花岗岩成因

构造岩浆作用

The Urucum suite (582 ± 2 Ma, zircon U-Pb age), situated in the Mid-Rio Doce Valley, eastern part of Minas Gerais State, is characterized by elongated, NW-SE and N-S trending granitic massifs associat

NIAID Data Ecosystem40

Late Cretaceous–Eocene magmatism induced by slab rollback and breakoff in the Tengchong terrane, SW China

花岗岩成因

构造板块运动

Late Cretaceous–Eocene granites are widespread in the Tengchong terrane and related to subduction and closure of the Neo–Tethyan Ocean. However, the reason of their compositional and spatial variation

Taylor & Francis Group2024-02-29 更新160

Data for: Magmatic recycling of accretionary wedge: a new perspective on Silurian-Devonian I-type granitoids generation in the Chinese Altai

构造岩浆作用

花岗岩成因

The supplementary Fig. S1 is classification of Silurian-Devonian granitods in the Chinese Altai. Fig. S2, S3 and S4 are supplements to Fig. 6 to dispaly chemical changes of the modelled melts with inc

Mendeley Data60

XHD-PSC-Supporting-Information-20191231.pdf

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