Abstract
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
| Original language | English |
|---|---|
| Pages (from-to) | 106-113 |
| Number of pages | 8 |
| Journal | Proceedings - Geological Society of China |
| Volume | 28 |
| Publication status | Published - 1985 Jan 1 |
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All Science Journal Classification (ASJC) codes
- Environmental Science(all)
- Earth and Planetary Sciences(all)
Cite this
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Analysis on graphitization of carbonaceous materials from the Chiao-Chi area and its implications ( China). / You, Chen-Feng; Shu-Cheng Yu, Yu.
In: Proceedings - Geological Society of China, Vol. 28, 01.01.1985, p. 106-113.Research output: Contribution to journal › Article
TY - JOUR
T1 - Analysis on graphitization of carbonaceous materials from the Chiao-Chi area and its implications ( China).
AU - You, Chen-Feng
AU - Shu-Cheng Yu, Yu
PY - 1985/1/1
Y1 - 1985/1/1
N2 - 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
AB - 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
UR - http://www.scopus.com/inward/record.url?scp=0022194611&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=0022194611&partnerID=8YFLogxK
M3 - Article
VL - 28
SP - 106
EP - 113
JO - Proceedings - Geological Society of China
JF - Proceedings - Geological Society of China
SN - 0431-2155
ER -