In situ mineral chemistry, geochronology, and isotope geochemistry of titanite, Nb–REE minerals, apatite, and biotite from the Baicao aplite–pegmatite system, Pan-Xi area

Creator(s):

Yin, Rong; ORCID: 0000-0002-8181-676X
Sun, Xiao-Ming
Wang, Sheng-Wei
Ran, Meng-Lan
Hu, Rui-Zhong
Huang, Xiao-Long

Abstract:

To constrain the magma source and unravel the roles of magmatic evolution and the subsequent magmatic–hydrothermal transition in the petrogenesis and Nb–REE mineralization of Permian plume-related NYF-type pegmatites, we conducted in situ mineral chemistry, geochronological, and isotope geochemical analyses of titanite, Nb–REE minerals, apatite, and biotite from the Baicao aplite and pegmatite in the Pan-Xi area.

How to cite this dataset:

Yin, R., Sun, X., Wang, S., Ran, M., Hu, R., Huang, X., 2026. In situ mineral chemistry, geochronology, and isotope geochemistry of titanite, Nb–REE minerals, apatite, and biotite from the Baicao aplite–pegmatite system, Pan-Xi area, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.60520/IEDA/114577. Accessed 2026-08-03.

DOI Creation Date:

2026-07-28

License:

Creative Commons Attribution 4.0 International [CC-BY-4.0]

Keyword(s):

Coverage Scope: Regional (Continents, Oceans)

User Contributed Keyword(s):

NYF-type pegmatite, fractional crystallization, titanite, Emeishan large igneous province, alkaline magmatism

Data Available On:

2026-07-31

Resource Type:

Collection

Dataset Information

DOI: 10.60520/IEDA/114577

In situ mineral chemistry, geochronology, and isotope geochemistry of titanite, Nb–REE minerals, apatite, and biotite from the Baicao aplite–pegmatite system, Pan-Xi area