DATA AVAILABILITY: Eocene and Miocene crustal thermal state of the eastern Gangdese belt: Insights into the formation mechanisms of post-collisional Cu-fertile magmas

Zhou et al., 2023. Eocene and Miocene crustal thermal state of the eastern Gangdese belt: Insights into the formation mechanisms of post-collisional Cu-fertile magmas. <i>Mineralium Deposita</i>.<br>Table S1. Compilations of major and trace elements of Eocene and Miocene magmatic rocks from the Gangdese belt.Table S2. Compilations of major and trace elements of Paleocene-Eocene, Cretaceous, and Jurassic mafic rocks from the Gangdese belt.Table S3. Average composition of potential source mafic rocks for Eocene and Miocene intermediate to felsic magmatic rocks.Table S4. Mineral partition coefficients used in trace element modelling of partial melting of mafic rocks.Table S5. Thermodynamic and trace element modelling of partial melting of Eocene and Miocene source rocks.

周等（Zhou et al.）, 2023。《冈底斯带（Gangdese Belt）东段始新世-中新世地壳热状态：碰撞后富铜岩浆的形成机制探析》，刊载于《矿床学》（Mineralium Deposita）。
附表S1：冈底斯带始新世-中新世岩浆岩主量与微量元素汇编数据。
附表S2：冈底斯带古新世-始新世、白垩纪及侏罗纪镁铁质岩主量与微量元素汇编数据。
附表S3：始新世-中新世中酸性岩浆岩潜在源区镁铁质岩的平均组成。
附表S4：镁铁质岩部分熔融微量元素模拟所用的矿物分配系数。
附表S5：始新世-中新世源区岩石部分熔融的热力学与微量元素模拟。