A Crustal Hot, Low-Resistivity Zone Caused by Late Paleozoic A-Type Granitoids in the Western Part of the Northern Margin of the North China Craton

Name: A Crustal Hot, Low-Resistivity Zone Caused by Late Paleozoic A-Type Granitoids in the Western Part of the Northern Margin of the North China Craton
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NIAID Data Ecosystem2026-05-02 收录

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https://zenodo.org/record/14716306

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资源简介：

Tables S1, a sheet presenting parameters for solving heat equation and one-dimensional numerical analysis for the A-type granites from the Northern margin of the NCC.

创建时间：

2025-01-22