Influence of volcanic activities to organic maturation in Jiufen-Chinkuashih Area.

碩士 === 國立中央大學 === 應用地質研究所 === 96 === ABSTRACT Influencing factors of vitrinite reflectance include heated temperature and time, volcanic and hydrothermal activities, tectonic and burial deposition, etc. Organic miscelles decompose after being heated and leading to the increase of vitrinite reflect...

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Main Authors: Yi-Cheng Lee, 黎易辰
Other Authors: Louis L. Tsai
Format: Others
Language:zh-TW
Published: 2008
Online Access:http://ndltd.ncl.edu.tw/handle/3as7sg
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spelling ndltd-TW-096NCU055030032019-05-15T19:18:55Z http://ndltd.ncl.edu.tw/handle/3as7sg Influence of volcanic activities to organic maturation in Jiufen-Chinkuashih Area. 九份-金瓜石地區火成作用對有機物成熟度之影響 Yi-Cheng Lee 黎易辰 碩士 國立中央大學 應用地質研究所 96 ABSTRACT Influencing factors of vitrinite reflectance include heated temperature and time, volcanic and hydrothermal activities, tectonic and burial deposition, etc. Organic miscelles decompose after being heated and leading to the increase of vitrinite reflectance. The influence of volcanic and hydrothermal activities is especially notice-worthy. Coal samples were collected from Jiufen-Jilong Shan and Fushan gold mine area in this study. Vitrinite reflectance and Rock-Eval pyrolysis were then performed to evaluate the influence of past igneous intrusion as well as hydrothermal deposits.Maximum and average heated temperature can thus be estimated. The results indicate that in the study area, Ro increased from 0.5-0.7% to 1.1-3.0% in the nearby of intruded igneous bodies, where as Ro increased up to 2.0~7.0% in areas close to hydrothermal ore deposits. Samples #1,3and4 were especially affected by hydrothermal deposits with Ro~5.59%. The heated temperatures were estimated as 500~600°C maximum and 460~560°C in average. Louis L. Tsai 蔡龍珆 2008 學位論文 ; thesis 64 zh-TW
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language zh-TW
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description 碩士 === 國立中央大學 === 應用地質研究所 === 96 === ABSTRACT Influencing factors of vitrinite reflectance include heated temperature and time, volcanic and hydrothermal activities, tectonic and burial deposition, etc. Organic miscelles decompose after being heated and leading to the increase of vitrinite reflectance. The influence of volcanic and hydrothermal activities is especially notice-worthy. Coal samples were collected from Jiufen-Jilong Shan and Fushan gold mine area in this study. Vitrinite reflectance and Rock-Eval pyrolysis were then performed to evaluate the influence of past igneous intrusion as well as hydrothermal deposits.Maximum and average heated temperature can thus be estimated. The results indicate that in the study area, Ro increased from 0.5-0.7% to 1.1-3.0% in the nearby of intruded igneous bodies, where as Ro increased up to 2.0~7.0% in areas close to hydrothermal ore deposits. Samples #1,3and4 were especially affected by hydrothermal deposits with Ro~5.59%. The heated temperatures were estimated as 500~600°C maximum and 460~560°C in average.
author2 Louis L. Tsai
author_facet Louis L. Tsai
Yi-Cheng Lee
黎易辰
author Yi-Cheng Lee
黎易辰
spellingShingle Yi-Cheng Lee
黎易辰
Influence of volcanic activities to organic maturation in Jiufen-Chinkuashih Area.
author_sort Yi-Cheng Lee
title Influence of volcanic activities to organic maturation in Jiufen-Chinkuashih Area.
title_short Influence of volcanic activities to organic maturation in Jiufen-Chinkuashih Area.
title_full Influence of volcanic activities to organic maturation in Jiufen-Chinkuashih Area.
title_fullStr Influence of volcanic activities to organic maturation in Jiufen-Chinkuashih Area.
title_full_unstemmed Influence of volcanic activities to organic maturation in Jiufen-Chinkuashih Area.
title_sort influence of volcanic activities to organic maturation in jiufen-chinkuashih area.
publishDate 2008
url http://ndltd.ncl.edu.tw/handle/3as7sg
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