摘要
X-ray experiments indicate that the carbonaceous samples are sub-graphitic in crystallinity and turbostratic in structure is 3.52A with the peak-width ratio of 1 indicating its d2 category based on Landis' classification. Indicates that the carbonaceous materials and the host rock formation were of non-marine deposits and later subjected to a low grade metamorphism at temperature between 300-350oC. -from Authors
原文 | English |
---|---|
頁(從 - 到) | 106-113 |
頁數 | 8 |
期刊 | Proceedings - Geological Society of China |
卷 | 28 |
出版狀態 | Published - 1985 |
All Science Journal Classification (ASJC) codes
- 環境科學 (全部)
- 地球與行星科學(全部)