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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:creator>Richard M. Pollastro</dc:creator>
  <dc:date>1999</dc:date>
  <dc:description>Three Total Petroleum Systems each&#13;
consisting of one assessment unit have been&#13;
identified in the Ghaba and Fahud Salt Basin&#13;
Provinces of north-central Oman. One Total&#13;
Petroleum System and corresponding assessment&#13;
unit, the North Oman Huqf/?Q??Haushi(!)&#13;
Total Petroleum System (201401) and Ghaba-&#13;
Makarem Combined Structural Assessment Unit&#13;
(20140101), were identified for the Ghaba Salt&#13;
Basin Province (2014). In the Fahud Salt Basin&#13;
Province, however, two overlapping Total&#13;
Petroleum Systems (TPS) were recognized: (1)&#13;
the North Oman Huqf?Shu?aiba(!) TPS&#13;
(201601); Fahud-Huqf Combined Structural&#13;
Assessment Unit (20160101), and (2) the middle&#13;
Cretaceous Natih(!) TPS (201602); Natih-Fiqa&#13;
Structural/Stratigraphic Assessment Unit&#13;
(20160201). The boundary for each Total&#13;
Petroleum System also defines the boundary of&#13;
the corresponding assessment unit and includes&#13;
all trap styles and hydrocarbon-producing&#13;
reservoirs within the petroleum system.&#13;
In both the Ghaba and Fahud Salt Basin&#13;
Provinces, hydrocarbons were generated from&#13;
several deeply buried source rocks within the&#13;
Infracambrian Huqf Supergroup. One general&#13;
?North Oman Huqf? type oil is dominant in the&#13;
Fahud Salt Basin. Oils in the Ghaba Salt&#13;
Basin are linked to at least two distinct Huqf&#13;
source-rock units based on oil geochemistry: a&#13;
general North Oman Huqf-type oil source and a&#13;
more dominant ?questionable unidentified&#13;
source? or ?Q?-type Huqf oil source. These two&#13;
Huqf-sourced oils are commonly found as&#13;
admixtures in reservoirs throughout northcentral&#13;
Oman.&#13;
Hydrocarbons generated from Huqf sources&#13;
are produced from a variety of reservoir types&#13;
and ages ranging from Precambrian to&#13;
Cretaceous in both the Ghaba and Fahud Salt&#13;
Basin Provinces. Clastic reservoirs of the&#13;
Gharif and Al Khlata Formations, Haushi&#13;
Group (middle Carboniferous to Lower&#13;
Permian), dominate oil production in the&#13;
Ghaba Salt Basin Province and form the basis&#13;
for the Huqf/?Q??Haushi(!) TPS. In contrast,&#13;
the Lower Cretaceous Shu?aiba and middle&#13;
Cretaceous Natih limestones account for most of&#13;
the production in the Fahud Salt Basin with&#13;
about 50 percent of the basin?s production from&#13;
porous, fractured Shu?aiba limestones in Yibal&#13;
field, thus the name North Oman Huqf?&#13;
Shu?aiba(!) TPS. Deep gas is produced mainly&#13;
from Middle Cambrian to Lower Ordovician&#13;
clastic reservoirs of the Haima Supergroup.&#13;
Traps in nearly all hydrocarbon accumulations&#13;
of these petroleum systems are mainly&#13;
structural and were formed by one or more&#13;
3&#13;
mechanisms. These trap-forming mechanisms&#13;
were mainly periodic halokinesis of the thick&#13;
Cambrian Ara Salt and consequent folding and&#13;
faulting from basin loading, rifting, or other&#13;
major tectonic events, particularly those events&#13;
forming the Oman Mountains and associated&#13;
foreland-basin system during the Late&#13;
Cretaceous and late Tertiary.&#13;
Many of the future new-field targets will&#13;
likely be low-relief, subtle structures, as many&#13;
of the large structures have been drilled.&#13;
Oman?s recent interest and commitments to&#13;
liquid natural gas export make deep gas a&#13;
primary objective in the two North Oman Huqf&#13;
petroleum systems. New-field exploration of&#13;
deep gas and exploring deeper targets for gas in&#13;
existing fields will likely identify a&#13;
significant gas resource in the next 30 years.&#13;
Moreover, salt-diapir flank traps in these two&#13;
North Oman Huqf petroleum systems and salt&#13;
basin provinces have gone essentially untested&#13;
and will likely be targeted in the near future.&#13;
The middle Cretaceous Natih(!) TPS is a&#13;
small efficient system of the Fahud Salt Basin.&#13;
Natih source rocks are only mature in the Late&#13;
Cretaceous/Tertiary foredeep and production is&#13;
primarily from Natih reservoirs; minor&#13;
production from the Shu?aiba limestone is&#13;
documented along fault-dip structures. Most&#13;
traps are structural and are related to&#13;
development of the foreland basin and&#13;
formation of the Oman Mountains. Future&#13;
targets of the Natih TPS will be less obvious&#13;
</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/b2167</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Dept. of the Interior, U.S. Geological Survey,</dc:publisher>
  <dc:title>Ghaba salt basin province and Fahud salt basin province, Oman; geological overview and total petroleum systems</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>