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題 名 | 不同成熟度碳氫化合物對比參數整合=Discussion on the Correlation Parameters of Hydrocarbon in Various Maturity |
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作 者 | 林政遠; 胡峻榕; 沈俊卿; 周次雄; 傅錦德; 莊福森; 張嘉福; | 書刊名 | 探採研究彙報 |
卷 期 | 20 1997.11[民86.11] |
頁 次 | 頁257-271 |
分類號 | 457.8 |
關鍵詞 | 碳同位素; 低溫成油作用; 熱動趨式; 異構物; 移棲量; Carbon isotope; Isomers; Quantity of second migration; |
語 文 | 中文(Chinese) |
中文摘要 | 以天然氣中各組成成份的特性,天然氣碳同位素值分佈,不僅可簡易區分天然氣 的氣源,而且可推測天然氣成熟度,進而建立天然氣移棲量的初步估算。油岩樣成熟度的測 定, 份以傳統方法為主, 生物指標較能完整的描述成熟度的特性; 本篇初步建立 D1(M/Z123) 與 C homohopane 及與 C �V sterane 之成熟度關係。 油岩樣碳同位素值應用 於熱成熟度的關係尚無明顯的突破;但應用於油氣移棲量的估算,本篇提出初步看法。天然 氣與油氣移棲量的估算皆為首次提出。 |
英文摘要 | Based on the Characteristics of various components, and the carbon isotope distribution in natural gas, gaseous phase of hydrocarbons canbe easily investigated not only for its source-derivation but also for the prediction of its maturity. In addition, Quantity of second migration for gaseous hydrocarbon from possible source rocks in Taiwan can be estimated based on the same factors. Traditional method, such as biomarkers parameter indices, still is the useful method for the hydrocarbons correlation between petroleum and source rock extracts up to now. The relationship of Diterpane (D1) with homohopane (C31) and with sterane (C29) in terrigenous source input are good for indicating maturity in Taiwan; however, application of velationship in carbon isotopes on estimating maturity is not very successful yet. |
本系統中英文摘要資訊取自各篇刊載內容。