| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6440793 | Lithos | 2014 | 16 Pages |
Abstract
Relative abundance of oceanic components in the Khao Chao gneiss, their Late Triassic magmatic ages, and the Early Jurassic metamorphic ages prefer the interpretation that the Khao Chao gneiss belongs to the Sukhothai Arc.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
T. Kawakami, N. Nakano, F. Higashino, T. Hokada, Y. Osanai, M. Yuhara, P. Charusiri, H. Kamikubo, K. Yonemura, T. Hirata,