Hydrocarbon accumulation and formation of composite reservoirs in KL16-1 of Laizhou Bay Sag, Bohai Sea, China

The Laizhou Bay Sag, one of the oil-bearing sags with large exploration potential in the South Bohai Sea of China, contains two sets of high-quality hydrocarbon source rocks, i.e. Member 3 and Member 4 of Shahejie Fm (E 2 s 3 and E 2 s 4 ). As an important hydrocarbon accumulation zone in the sag, t...

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Main Authors: Yunlong Xu, Xiaoping Luo, Ajuan Wei, Mingcai Hou, Haoming Wu, Yong Li
Format: Article
Language:English
Published: SAGE Publishing 2018-11-01
Series:Energy Exploration & Exploitation
Online Access:https://doi.org/10.1177/0144598718760899
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spelling doaj-d558d7b1e4644fc1a6f12263704f356f2020-11-25T04:08:22ZengSAGE PublishingEnergy Exploration & Exploitation0144-59872048-40542018-11-013610.1177/0144598718760899Hydrocarbon accumulation and formation of composite reservoirs in KL16-1 of Laizhou Bay Sag, Bohai Sea, ChinaYunlong XuXiaoping LuoAjuan WeiMingcai HouHaoming WuYong LiThe Laizhou Bay Sag, one of the oil-bearing sags with large exploration potential in the South Bohai Sea of China, contains two sets of high-quality hydrocarbon source rocks, i.e. Member 3 and Member 4 of Shahejie Fm (E 2 s 3 and E 2 s 4 ). As an important hydrocarbon accumulation zone in the sag, the KL16-1 low bulge is found to have oil reservoirs in the Neogene Guantao Fm (N 1 g), the Paleogene Dongying Fm (E 3 d), the Paleogene Shahejie Fm (E 2 s), and the Mesozoic buried hill formation. It is characterized by distinct features of composite reservoirs. Nonetheless, its hydrocarbon accumulation process and mechanism are unknown yet. In this paper, the hydrocarbon generation modelling of source rocks, combined with the characteristics of oil-source rock biomarker compounds and fluid inclusions, is used to restore the hydrocarbon accumulation process in the KL16-1 low bulge. Crude oil in all three KL16-1 plays is characterized by low Pr/Ph, low gammacerane, high 4-methyl sterane and high dinosterane. In other words, it is oil of low maturity to maturity. As the biomarker index of the oil is very similar to that of the E 2 s 3 source rocks, it is thought that E 2 s 3 is the primary source rock layer, while E 2 s 4 is the secondary source rock layer. In addition, episodic oil and gas charging happened in two phases under high pressure in the late period (from 5.0 Ma till now).https://doi.org/10.1177/0144598718760899
collection DOAJ
language English
format Article
sources DOAJ
author Yunlong Xu
Xiaoping Luo
Ajuan Wei
Mingcai Hou
Haoming Wu
Yong Li
spellingShingle Yunlong Xu
Xiaoping Luo
Ajuan Wei
Mingcai Hou
Haoming Wu
Yong Li
Hydrocarbon accumulation and formation of composite reservoirs in KL16-1 of Laizhou Bay Sag, Bohai Sea, China
Energy Exploration & Exploitation
author_facet Yunlong Xu
Xiaoping Luo
Ajuan Wei
Mingcai Hou
Haoming Wu
Yong Li
author_sort Yunlong Xu
title Hydrocarbon accumulation and formation of composite reservoirs in KL16-1 of Laizhou Bay Sag, Bohai Sea, China
title_short Hydrocarbon accumulation and formation of composite reservoirs in KL16-1 of Laizhou Bay Sag, Bohai Sea, China
title_full Hydrocarbon accumulation and formation of composite reservoirs in KL16-1 of Laizhou Bay Sag, Bohai Sea, China
title_fullStr Hydrocarbon accumulation and formation of composite reservoirs in KL16-1 of Laizhou Bay Sag, Bohai Sea, China
title_full_unstemmed Hydrocarbon accumulation and formation of composite reservoirs in KL16-1 of Laizhou Bay Sag, Bohai Sea, China
title_sort hydrocarbon accumulation and formation of composite reservoirs in kl16-1 of laizhou bay sag, bohai sea, china
publisher SAGE Publishing
series Energy Exploration & Exploitation
issn 0144-5987
2048-4054
publishDate 2018-11-01
description The Laizhou Bay Sag, one of the oil-bearing sags with large exploration potential in the South Bohai Sea of China, contains two sets of high-quality hydrocarbon source rocks, i.e. Member 3 and Member 4 of Shahejie Fm (E 2 s 3 and E 2 s 4 ). As an important hydrocarbon accumulation zone in the sag, the KL16-1 low bulge is found to have oil reservoirs in the Neogene Guantao Fm (N 1 g), the Paleogene Dongying Fm (E 3 d), the Paleogene Shahejie Fm (E 2 s), and the Mesozoic buried hill formation. It is characterized by distinct features of composite reservoirs. Nonetheless, its hydrocarbon accumulation process and mechanism are unknown yet. In this paper, the hydrocarbon generation modelling of source rocks, combined with the characteristics of oil-source rock biomarker compounds and fluid inclusions, is used to restore the hydrocarbon accumulation process in the KL16-1 low bulge. Crude oil in all three KL16-1 plays is characterized by low Pr/Ph, low gammacerane, high 4-methyl sterane and high dinosterane. In other words, it is oil of low maturity to maturity. As the biomarker index of the oil is very similar to that of the E 2 s 3 source rocks, it is thought that E 2 s 3 is the primary source rock layer, while E 2 s 4 is the secondary source rock layer. In addition, episodic oil and gas charging happened in two phases under high pressure in the late period (from 5.0 Ma till now).
url https://doi.org/10.1177/0144598718760899
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