2010GeochimicaRequires access

Origin of Chang 10 oil reservoir in Northern Shaanxi region of Ordos Basin

Wu Kai

Open publisher page 5 citations

Abstract

The Chang 10 oil reservoir was discovered through the exploration in the Zhidan region of Ordos Basin, where the crude shows a density of 0. 8152 g /cm3 and a main peak at nC15 in the whole hydrocarbon chromatogram. The crude consists mainly of light hydrocarbons, which include abundant naphthenic hydrocarbons and low content of aromatic hydrocarbons, and has an equilibrial ratio of Pr / Ph, varing from 1. 21 to 1. 45, and - 31. 78‰ of δ13CPDB for the whole crude. Its terpane distribution is characterized by relatively abundant rearranged hopanes, low content of gammacerane, and high ratios of Ts /Tm (5. 54 - 7. 26), C30* /C30 hopane (0. 67 - 0. 72), and C29Ts / C30 hopane (0. 38 - 0. 52). The steranes in the crude mainly consist of rearranged steranes, and show abundant αβ and βα isomers, while ααα-20R sterane isomers display an asymmetricVtype distribution pattern, representing a typical lacustrine-derived oil. The oil-oil and oil-source correlations indicate that the crude oil of Chang 10 oil reservoir is originated from the excellent hydrocarbon source rocks of the Chang 7 member in the center of the basin, and migrated vertically into the Chang 10 oil layer, and then accumulated laterally. Therefore, it can be predicted that the Chang 9 and Chang 10 oil reservoirs in the Ordos Basin have favorable reservoir-forming conditions and great potential for exploration.

About this research paper

What this paper is about

The Chang 10 oil reservoir was discovered through the exploration in the Zhidan region of Ordos Basin, where the crude shows a density of 0. 8152 g /cm3 and a main peak at nC15 in the whole hydrocarbon chromatogram. The crude consists mainly of light hydrocarbons, which include abundant naphthenic hydrocarbons and low content of aromatic hydrocarbons, and has an equilibrial ratio of Pr / Ph, varing from 1. 21 to 1. 45, and - 31. 78‰ of δ13CPDB for the whole crude. Its terpane distribution is characterized by relatively abundant rearranged hopanes, low content of gammacerane, and high ratios of Ts /Tm (5. 54 - 7. 26), C30* /C30 hopane (0. 67 - 0. 72), and C29Ts / C30 hopane (0. 38 - 0. 52). The steranes in the crude mainly consist of rearranged steranes, and show abundant αβ and βα isomers, while ααα-20R sterane isomers display an asymmetricVtype distribution pattern, representing a typical lacustrine-derived oil. The oil-oil and oil-source correlations indicate that the crude oil of Chang 10 oil reservoir is originated from the excellent hydrocarbon source rocks of the Chang 7 member in the center of the basin, and migrated vertically into the Chang 10 oil layer, and then accumulated laterally. Therefore, it can be predicted that the Chang 9 and Chang 10 oil reservoirs in the Ordos Basin have favorable reservoir-forming conditions and great potential for exploration.

Why it matters

OpenAlex reports 5 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

The Chang 10 oil reservoir was discovered through the exploration in the Zhidan region of Ordos Basin, where the crude shows a density of 0. 8152 g /cm3 and a main peak at nC15 in the whole hydrocarbon chromatogram. The crude consists mainly of light hydrocarbons, which include abundant naphthenic hydrocarbons and low content of aromatic hydrocarbons, and has an equilibrial ratio of Pr / Ph, varing from 1. 21 to 1. 45, and - 31. 78‰ of δ13CPDB for the whole crude. Its terpane distribution is characterized by relatively abundant rearranged hopanes, low content of gammacerane, and high ratios of Ts /Tm (5. 54 - 7. 26), C30* /C30 hopane (0. 67 - 0. 72), and C29Ts / C30 hopane (0. 38 - 0. 52). The steranes in the crude mainly consist of rearranged steranes, and show abundant αβ and βα isomers, while ααα-20R sterane isomers display an asymmetricVtype distribution pattern, representing a typical lacustrine-derived oil. The oil-oil and oil-source correlations indicate that the crude oil of Chang 10 oil reservoir is originated from the excellent hydrocarbon source rocks of the Chang 7 member in the center of the basin, and migrated vertically into the Chang 10 oil layer, and then accumulated laterally. Therefore, it can be predicted that the Chang 9 and Chang 10 oil reservoirs in the Ordos Basin have favorable reservoir-forming conditions and great potential for exploration.

Key concepts: Hopanoids, Sterane, Source rock, Hydrocarbon, Geology, Crude oil, Structural basin, Light crude oil

Related papers

Back to paper searchBrowse research topicsOriginal source
Origin of Chang 10 oil reservoir in Northern Shaanxi region of Ordos Basin — Research Paper | ScholarLens