scholarly journals Supplemental Material: Magmatic record of continuous Neo-Tethyan subduction after initial India-Asia collision in the central part of southern Tibet

Author(s):  
Feng Huang ◽  
et al.

Analytical methods, data (Tables S1–S4), and modeling results (Tables S5–S6).

2020 ◽  
Author(s):  
Feng Huang ◽  
et al.

Analytical methods, data (Tables S1–S4), and modeling results (Tables S5–S6).


2020 ◽  
Author(s):  
Feng Huang ◽  
et al.

Analytical methods, data (Tables S1–S4), and modeling results (Tables S5–S6).


2020 ◽  
Author(s):  
Yue Qi ◽  
QIANG WANG ◽  
et al.

Analytical methods, field geological cross-section, and analytical results for the Lopu Range batholith from southern Tibet.


2021 ◽  
Author(s):  
Daoliang Chu ◽  
et al.

Description of the studied borehole, analytical methods, supplemental figure, and data tables.<br>


2020 ◽  
Author(s):  
Lyle Nelson ◽  
et al.

Detailed analytical methods, compiled geochronology data and references, U-Pb geochronology data tables, and field and petrographic photographs.<br>


2022 ◽  
Author(s):  
Alexie E.G. Millikin ◽  
et al.

Detailed analytical methods and sample information, data tables containing all geochemical data, and compiled geochronological and chemostratigraphic data.<br>


2021 ◽  
Author(s):  
Daoliang Chu ◽  
et al.

Description of the studied borehole, analytical methods, supplemental figure, and data tables.<br>


2022 ◽  
Author(s):  
Chao Wang ◽  
et al.

Text S1: Analytical methods. Figure S1: Zr versus selected element variation diagrams to highlight the effects of alteration and metamorphism for the basalts from Langjiexue area. Figure S2: (A) Ti/Y vs. TiO2, and (B) Ti/Y vs. MgO diagrams for the basalt samples from the Langjiexue in Tethyan Himalaya. Table S1: Representative Permian-Triassic magmatic events along the Tethyan Himalaya. Table S2: Zircon LA-ICP-MS U-Pb in-situ analyzing results for zircons from the Langjiexue basalts. Table S3: Whole-rock major, trace element and Sr-Nd isotope data of Langjiexue basalts.


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