LITHOS

Table S1 A summary of the Eartly Paleozoic granitoids in the Western Kunlun orogen. Table S2. Zircon U-Pb isotopic and REE concentrations obtained by LA-ICP-MS for samples from the Sanshili and Yirba plutons. Table S3. Lu-Hf isotope compositions of zircons form the Sanshili and Yirba plutons. Table S4 Major element, trace element and isotopic compositions of the Sanshili and Yirba plutons.

Supplementary data table S1-7.

Chemical composition of Jurassic granites of the Sanandaj-Sirjan Zone, western Iran

Whole-rock platinum group elements contents of Zunhua podiform chromitites; major, minor, and trace elements content of chromite grains in Zunhua podiform chromitites

These data include major and trace element compositions, zircon ages and Hf-isotope compositions of the early Paleozoic Chu Lai and Dai Loc granitic complexes in the Kontum Massif, central Vietnam. They are used to determine the formation ages, origins, source compositions and tectonic settings of these two granitc complexes, and in turn reveal the early Paleozoic tectonic evolution of the eastern Indochina Block, and relationship with other continents along the northern margin of the Gondwana.

We provide major and trace elements, zircon U-Pb ages and Hf isotopes for the Baijianshan high-Mg diorites and Dawanbei and Dabanxi A-type rhyolites.

The major element, trace element and Sr isotope compositions for plagioclase analyzed by EMP, LA-ICP-MS and LA-MC-ICPMS.

In this study, we present new geochemical (whole-rock major and trace element), isotopic (Rb-Sr and Sm-Nd) and geochronological (U-Pb) data from the Kuh-e-Shah volcanic rocks with a comparison to other scattered volcanic rocks throughout the Lut Block (Pang et al., 2013; Saadat & Stern, 2016; Javidi Moghaddam et al., 2019) in order to better understanding the Paleogene magmatism evolution of the Lut Block and to place constraints to the timing and onset of volcanism, its tectonic implications, the geochemical features of the mantle source involved in volcanic rocks genesis, petrogenetic processes and the controls of magma generation processes, the probable effects of fractional crystallization and crustal contamination, and geodynamic evolution of volcanic rocks which exposed in the western part of the Kuh-e-Shah volcano-plutonic complex.

Raw data of zircon O isotope

Supplementary Table 1. Zircon U–Pb dating data for the late Permian–Triassic igneous rocks in the Bureya Massif Supplementary Table 2. Major (wt.%) and trace (ppm) elements for the late Permian–Triassic igneous rocks in the Bureya Massif Supplementary Table 3. Zircon Hf isotope data for the late Permian–Triassic igneous rocks in the Bureya Massif