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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Characterization of hydrothermally generated oil from the Uzon caldera, Kamchatka
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Characterization of hydrothermally generated oil from the Uzon caldera, Kamchatka

机译:堪察加乌松火山口的热液生成油的表征

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This paper reports the analyses of unusual oils that accumulate in the Uzon Caldera, situated in the central volcanic region of Kamchatka, Russia. Gas chromatography-mass spectrometry (GC-MS) was used to determine the primary constituents, and the C-13 and C-14 compositions provided information about the potential source and age of the oils. The C-14 ages determined are 1030 +/- 40 a BP (measured) or 940 40 a BP (conventional). The delta C-13 value is -30.6 parts per thousand versus the PDB standard, a value consistent with a biological origin. The nearly contemporary age of the C content indicates a geologically recent origin from biogenic detritus and not by synthesis from mantle C. The biogenic origin is supported by the presence of sterane and hopane biomarkers and the delta C-13 value of the bulk oil. The overall compositions of the oils indicate that they are derived from rapid hydrothermal alteration of algal/bacterial mat detritus buried by volcanic ashfall deposits of the Uzon Caldera. The oils represent the youngest hydrothermal petroleum reported to date. (c) 2008 Elsevier Ltd. All rights reserved.
机译:本文报告了对位于俄罗斯堪察加半岛中部火山区的乌松火山口中聚集的异常油的分析。气相色谱-质谱法(GC-MS)用于确定主要成分,C-13和C-14组成提供了有关油的潜在来源和使用年限的信息。确定的C-14年龄为1030 +/- 40 a BP(实测)或940 40 a BP(常规)。相对于PDB标准,ΔC-13值为-30.6千分之几,与生物学来源一致。碳含量的近代年龄表明,地质学上起源于生物碎屑,而不是地幔C合成。生物成因得到了甾烷和hop烷生物标记物的存在以及散装油的C-13值的支持。油的总体组成表明,它们是由乌宗破火山口的火山灰沉积物掩埋的藻类/细菌垫碎屑的快速水热蚀变而得。这些油是迄今为止报道的最年轻的热液石油。 (c)2008 Elsevier Ltd.保留所有权利。

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