Knowledge Management System Of Guangzhou Institute of Geochemistry，CAS
| 丁自耕; 仝来喜; 刘小汉; 刘兆; 周学君 | |
| 西藏定结高压基性麻粒岩(退变榴辉岩)的变质P-T轨迹及构造意义 | |
| Source Publication | 地球科学
 |
| ISSN | 1000-2383 |
| 2018 | |
| Volume | 43Issue:01Pages:220-235 |
| DOI | 10.3799/dqkx.2018.013 |
| Language | 中文 |
| Indexed By | EI |
| Citation statistics | |
| Document Type | 期刊论文 |
| Identifier | http://ir.gig.ac.cn/handle/344008/36366 |
| Collection | 同位素地球化学国家重点实验室 |
| Recommended Citation GB/T 7714 | 丁自耕,仝来喜,刘小汉,等. 西藏定结高压基性麻粒岩(退变榴辉岩)的变质P-T轨迹及构造意义[J]. 地球科学,2018,43(01):220-235. |
| APA | 丁自耕,仝来喜,刘小汉,刘兆,&周学君.(2018).西藏定结高压基性麻粒岩(退变榴辉岩)的变质P-T轨迹及构造意义.地球科学,43(01),220-235. |
| MLA | 丁自耕,et al."西藏定结高压基性麻粒岩(退变榴辉岩)的变质P-T轨迹及构造意义".地球科学 43.01(2018):220-235. |
| Files in This Item: | ||||||
| File Name/Size | DocType | Version | Access | License | ||
| 18582.pdf（4151KB） | 期刊论文 | 出版稿 | 开放获取 | CC BY-NC-SA | View Application Full Text | |
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