Petroleum geology and exploration in Levant Basin, Eastern Mediterranean

This paper analyzes hydrocarbon accumulation conditions, defines hydrocarbon plays and discusses their hydrocarbon accumulation models using geological and geophysical data and an international petroleum exploration and production database, with an approach of integrated geological investigation and...

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Main Authors: Kun TIAN, Jinyin YIN, Dapeng WANG, Jinrui GUO, Chongzhi TAO
Format: Article
Language:zho
Published: Editorial Office of Petroleum Geology and Experiment 2020-01-01
Series:Shiyou shiyan dizhi
Subjects:
Online Access:https://www.sysydz.net/cn/article/doi/10.11781/sysydz202001095
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author Kun TIAN
Jinyin YIN
Dapeng WANG
Jinrui GUO
Chongzhi TAO
author_facet Kun TIAN
Jinyin YIN
Dapeng WANG
Jinrui GUO
Chongzhi TAO
author_sort Kun TIAN
collection DOAJ
description This paper analyzes hydrocarbon accumulation conditions, defines hydrocarbon plays and discusses their hydrocarbon accumulation models using geological and geophysical data and an international petroleum exploration and production database, with an approach of integrated geological investigation and play quick analysis. The intention is to identify favorable areas for exploration in the Levant Basin which experienced three main tectonic evolution stages, including rifting, passive continental marginal and tectonic inversion. It can be divided into three plays in Miocene, Pliocene and Mesozoic reservoirs. The Miocene play is the most important. The controlling factors of Miocene play are Oligocene-Miocene biogenic gas, high-quality submarine fan turbidite sand reservoir that related to Palaeo-Nile drainage system, large-scale anticline traps formed during tectonic inversion and Messinian evaporite as a regional caprock. High-quality channel turbidite sand reservoirs related to small-medium sized submarine canyons and short-distance gas migration are key factors that control hydrocarbon accumulation of the Pliocene play. Potential Cretaceous deepwater clastics and Jurassic carbonate build-ups on highs comprise a speculative Mesozoic play in deep water. Three plays are favorable regimes for future exploration, and the Miocene play in deep water and the under-explored Mesozoic regime are of high exploration potential.
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spelling doaj.art-d6ac2b2c655a4e7d94ee230e73207f9d2024-03-05T04:45:23ZzhoEditorial Office of Petroleum Geology and ExperimentShiyou shiyan dizhi1001-61122020-01-014219510210.11781/sysydz202001095sysydz-42-1-95Petroleum geology and exploration in Levant Basin, Eastern MediterraneanKun TIAN0Jinyin YIN1Dapeng WANG2Jinrui GUO3Chongzhi TAO4SINOPEC Petroleum Exploration & Production Research Institute, Beijing 100083, ChinaSINOPEC Petroleum Exploration & Production Research Institute, Beijing 100083, ChinaSINOPEC Petroleum Exploration & Production Research Institute, Beijing 100083, ChinaSINOPEC Petroleum Exploration & Production Research Institute, Beijing 100083, ChinaSINOPEC Petroleum Exploration & Production Research Institute, Beijing 100083, ChinaThis paper analyzes hydrocarbon accumulation conditions, defines hydrocarbon plays and discusses their hydrocarbon accumulation models using geological and geophysical data and an international petroleum exploration and production database, with an approach of integrated geological investigation and play quick analysis. The intention is to identify favorable areas for exploration in the Levant Basin which experienced three main tectonic evolution stages, including rifting, passive continental marginal and tectonic inversion. It can be divided into three plays in Miocene, Pliocene and Mesozoic reservoirs. The Miocene play is the most important. The controlling factors of Miocene play are Oligocene-Miocene biogenic gas, high-quality submarine fan turbidite sand reservoir that related to Palaeo-Nile drainage system, large-scale anticline traps formed during tectonic inversion and Messinian evaporite as a regional caprock. High-quality channel turbidite sand reservoirs related to small-medium sized submarine canyons and short-distance gas migration are key factors that control hydrocarbon accumulation of the Pliocene play. Potential Cretaceous deepwater clastics and Jurassic carbonate build-ups on highs comprise a speculative Mesozoic play in deep water. Three plays are favorable regimes for future exploration, and the Miocene play in deep water and the under-explored Mesozoic regime are of high exploration potential.https://www.sysydz.net/cn/article/doi/10.11781/sysydz202001095petroleum geological characteristicsplayhydrocarbon accumulation modelexploration directionlevant basin
spellingShingle Kun TIAN
Jinyin YIN
Dapeng WANG
Jinrui GUO
Chongzhi TAO
Petroleum geology and exploration in Levant Basin, Eastern Mediterranean
Shiyou shiyan dizhi
petroleum geological characteristics
play
hydrocarbon accumulation model
exploration direction
levant basin
title Petroleum geology and exploration in Levant Basin, Eastern Mediterranean
title_full Petroleum geology and exploration in Levant Basin, Eastern Mediterranean
title_fullStr Petroleum geology and exploration in Levant Basin, Eastern Mediterranean
title_full_unstemmed Petroleum geology and exploration in Levant Basin, Eastern Mediterranean
title_short Petroleum geology and exploration in Levant Basin, Eastern Mediterranean
title_sort petroleum geology and exploration in levant basin eastern mediterranean
topic petroleum geological characteristics
play
hydrocarbon accumulation model
exploration direction
levant basin
url https://www.sysydz.net/cn/article/doi/10.11781/sysydz202001095
work_keys_str_mv AT kuntian petroleumgeologyandexplorationinlevantbasineasternmediterranean
AT jinyinyin petroleumgeologyandexplorationinlevantbasineasternmediterranean
AT dapengwang petroleumgeologyandexplorationinlevantbasineasternmediterranean
AT jinruiguo petroleumgeologyandexplorationinlevantbasineasternmediterranean
AT chongzhitao petroleumgeologyandexplorationinlevantbasineasternmediterranean