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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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Central Africa
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Central African Republic (1)
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Chad Basin (1)
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West Pacific
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Brazil
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nitrogen
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oxygen
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O-18/O-16 (1)
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sulfur
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fossils
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Invertebrata
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Insecta (1)
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Protista
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microfossils
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Plantae
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Spermatophyta
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geochronology methods
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Tertiary
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Shahejie Formation (4)
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Coal Measures (1)
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La Luna Formation (2)
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Pucara Group (1)
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Shublik Formation (1)
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Paleozoic
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Berea Sandstone (2)
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Carboniferous
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Lower Carboniferous
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Mississippian
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Madison Group (3)
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Sunbury Shale (1)
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Upper Mississippian
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Heath Formation (1)
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Pennsylvanian
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Smithwick Shale (1)
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Upper Carboniferous
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Chattanooga Shale (1)
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Devonian
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Winnipegosis Formation (1)
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Upper Devonian
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Leduc Formation (1)
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Grosmont Formation (1)
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Huron Member (1)
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Nisku Formation (2)
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Ohio Shale (2)
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Exshaw Formation (1)
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Horton Group (1)
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Hunton Group (1)
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Knox Group (1)
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Lisburne Group (1)
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lower Paleozoic
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Cape Phillips Formation (1)
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Ordovician
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Permian
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Upper Permian
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Zechstein (1)
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Silurian
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Middle Silurian
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Upper Silurian
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Salina Group (1)
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upper Paleozoic
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Bakken Formation (3)
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Woodford Shale (4)
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Precambrian
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upper Precambrian
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Proterozoic
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Mesoproterozoic (1)
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igneous rocks
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volcanic rocks
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volcanic ash (1)
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metamorphic rocks
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minerals
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sulfides
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galena (1)
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pyrite (2)
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sphalerite (2)
-
-
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Primary terms
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absolute age (2)
-
Africa
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Central Africa
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Central African Republic (1)
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Chad Basin (1)
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Congo Basin (2)
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North Africa
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West Africa
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Chad (1)
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Niger (2)
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Nigeria
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Far East
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-
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China
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Liaohe Field (1)
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Meishan China (1)
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Shandong China
-
Dongying Depression (1)
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Tancheng-Lujiang Fault (1)
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Xinjiang China
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Indonesia
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Kamchatka Russian Federation
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Krasnoyarsk Russian Federation
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Khanty-Mansi Russian Federation
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Samotlor Field (1)
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West Siberia
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Siberian Lowland (1)
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Yakutia Russian Federation
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Olenek River (1)
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Udachnaya Pipe (1)
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Yenisei-Khatanga basin (1)
-
-
Atlantic Ocean
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North Atlantic
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Gulf of Mexico
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Mississippi Canyon (1)
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Hudson Bay (1)
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Hudson Strait (1)
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Labrador Sea (1)
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North Sea
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Oseberg Field (1)
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Troll Field (1)
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South Atlantic
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Atlantic Ocean Islands
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Australasia
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Canada
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Western Canada
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British Columbia
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hopanes
Biomarker Evidence of Shifts in Organic Provenance and Depositional Environments of Eocene Carbonaceous Rocks from Petroliferous Barmer Basin, Western Rajasthan, India
Oil-source correlation in the Yangjiang Uplift, South China Sea: A comparative analysis of mathematical and fingerprint methods
DYNAMICS OF DEPOSITION AND FOSSIL PRESERVATION AT THE EARLY EOCENE OKANAGAN HIGHLANDS OF BRITISH COLUMBIA, CANADA: INSIGHTS FROM ORGANIC GEOCHEMISTRY
The Source of Organic Matter and Its Role in Producing Reduced Sulfur for the Giant Sediment-Hosted Jinding Zinc-Lead Deposit, Lanping Basin, Yunnan, Southwest China
A review of the Bakken petroleum systems in the United States and Canada: Recognizing the importance of the Middle Member play
Organic geochemistry and petrology of Devonian shale in eastern Ohio: Implications for petroleum systems assessment
Oil–source correlation studies in the shallow Berea Sandstone petroleum system, eastern Kentucky
Geochemistry of high-maturity crude oil and gas from deep reservoirs and their geological significance: A case study on Shuntuoguole low uplift, Tarim Basin, western China
An integrated organic–inorganic geochemical characterization of Paleogene sediments in No.1 Structural Belt of the Nanpu Sag, Bohai Bay Basin, eastern China: implications for the origin of organic matter
Making oil from magma
Abstract Petroleum systems within rifted margin basins affected by volcanism continue to remain challenging for the exploration of hydrocarbons, most notably owing to the volume of intrusions that pose imaging, drilling and exploration problems. Typically, intrusions possess small thermal aureoles, but despite this, there is evidence that intrusions could none the less be responsible for the generation of commercial volumes of hydrocarbons. Here we shed new light on this petroleum systems challenge by integrating organic geochemical and Raman spectroscopic techniques to produce potential volumetric data for hydrocarbons generated as a result of igneous intrusion. The results indicate that, in areas with immature source rock intervals, it may be possible for intrusions to generate volumes of oil that would be capable of comfortably filling likely known oil reservoirs. This is a critical step forward in integrating several analytical techniques, indicating that under the right conditions there is the potential for hydrocarbon generation as a result of igneous intrusion.