Comparison of I/S Transformation and Maturity of Organic Matter at Elevated Temperatures
Comparison of I/S Transformation and Maturity of Organic Matter at Elevated Temperatures
复制标题
高温下有机物 I/S 转化和成熟度的比较
DOI：
10.1346/ccmn.1993.0410206
复制
发表时间：
1993
影响因子：
2.2
通讯作者：
B. Lanson
中科院分区：
文献类型：
--
作者：
B. Velde;B. Lanson
Comparing the state of reaction advancement of I/S (illite content of illite/smectite mixed layer minerals) and organic matter (vitrinite reflectance) in instances of high temperature gradients allows one to observe the evolution of geologic materials under extreme conditions. In a geothermally heated sedimentary series (Salton Sea area, California), both clays and organics have reacted to completion in the temperature gradient range of 200°-400oC/km during heating episodes of 104 years. We observed an instance of rapid heating, through magmatic intrusion into the Meso-Paleozoic eastern Paris Basin sedimentary series in late Permian time, which induced changes in the organic material, but where clays are apparently unaffected.
影响因子：
3.5
作者：
J. Sweeney;A. Burnham
通讯作者：
J. Sweeney;A. Burnham