Please use this identifier to cite or link to this item: https://hdl.handle.net/11499/6726
Title: Geochemical overview and undiscovered gas resources generated from Hamitabat petroleum system in the Thrace Basin, Turkey
Authors: Gürgey, K.
Keywords: Eocene
Gas resources
Geochemistry
Petroleum system
Thrace Basin
Early miocene
Essential elements
Gas generations
Gaseous hydrocarbons
Hydrocarbon generations
Hydrocarbon resources
Oil and gas fields
Regional distributions
Source rocks
Thermal models
Vertical migrations
Energy resources
Gas industry
Gases
Meats
Oil fields
Organic compounds
Petroleum geology
Petroleum reservoirs
Shale
Gas condensates
gas condensate
gas field
geochemistry
hydrocarbon generation
hydrocarbon migration
hydrocarbon reservoir
hydrocarbon resource
Miocene
oil field
source rock
Eurasia
Europe
Isparta [Turkey]
Turkey
Abstract: Since the first drill in 1957, three oil, 19 gas and condensate fields have been discovered in the Thrace Basin. However, any petroleum system with its essential elements and processes has not been assigned yet. This study consists of two parts, (1) geochemical overview of the previous work in order to get a necessary help to construct a petroleum system and (2) calculation of quantitative undiscovered hydrocarbon resources generated from this system. An extensive overview study showed that the primary reservoir and source rocks in the Thrace Basin are the Middle Eocene Hamitabat sandstones and shales, respectively, hence it appears that the most effective petroleum system of the Thrace Basin becomes the Hamitabat (!) petroleum system. Currently, 18.5 billion m3 of in-place gas, 2.0 million m3 (12.7 million bbl) in-place waxy oil as well as minor amount of associated condensate were discovered from this system. This study showed that the regional distribution of the oil and gas fields almost overlapped with the previously constructed pod of active Hamitabat shales implying that short and up-dip vertical migration pathway of hydrocarbons from the source to trapping side was available. Thermal model demonstrated that hydrocarbon generation from the Hamitabat shales commenced in the Early Miocene. The amount of quantitative gas generation based on the mean-original TOC = 0.94 wt%, mean-original HI = 217 HC/g TOC and the volume of the pod of active source rock = 49 km3 is approximately 110 billion m3 of gaseous hydrocarbons that results in a high generation-accumulation efficiency of 17% when 18.5 billion m3 of already discovered hydrocarbons are considered. © 2008 Elsevier Ltd. All rights reserved.
URI: https://hdl.handle.net/11499/6726
https://doi.org/10.1016/j.marpetgeo.2008.08.007
ISSN: 0264-8172
Appears in Collections:Mühendislik Fakültesi Koleksiyonu
Scopus İndeksli Yayınlar Koleksiyonu / Scopus Indexed Publications Collection
WoS İndeksli Yayınlar Koleksiyonu / WoS Indexed Publications Collection

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