- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
-
Atlantic Ocean
-
North Atlantic
-
Gulf of Mexico (1)
-
Jeanne d'Arc Basin (1)
-
Northwest Atlantic (2)
-
-
-
Atlantic region (2)
-
Canada
-
Eastern Canada
-
Maritime Provinces
-
Nova Scotia
-
Minas Basin (2)
-
-
-
-
-
Europe
-
Southern Europe
-
Italy (1)
-
-
Western Europe
-
United Kingdom
-
Great Britain
-
England
-
Somerset England (2)
-
South-West England (2)
-
-
-
-
-
-
Hartford Basin (10)
-
North America
-
Appalachian Basin (1)
-
Appalachians
-
Hudson Highlands (1)
-
-
Keweenawan Rift (1)
-
Michigan Basin (1)
-
-
Palisades Sill (1)
-
Richmond Basin (5)
-
Rome Trough (1)
-
United States
-
Arizona (1)
-
Arkoma Basin (1)
-
Atlantic Coastal Plain (6)
-
Connecticut
-
Hartford County Connecticut (2)
-
New Haven County Connecticut (3)
-
-
Culpeper Basin (5)
-
Dan River basin (1)
-
Eastern U.S. (13)
-
Florida
-
South Florida Basin (1)
-
-
Gettysburg Basin (1)
-
Great Smoky Mountains (1)
-
Hudson Valley (1)
-
Illinois Basin (1)
-
Kansas
-
Sedgwick Basin (1)
-
-
Kentucky
-
Rough Creek fault zone (1)
-
-
Massachusetts (2)
-
Mississippi Embayment (1)
-
Narragansett Basin (1)
-
New England (2)
-
New Jersey
-
Hunterdon County New Jersey (1)
-
Mercer County New Jersey (2)
-
Middlesex County New Jersey (1)
-
Morris County New Jersey (4)
-
Somerset County New Jersey (3)
-
Warren County New Jersey (1)
-
Watchung Mountains (1)
-
-
New Mexico (1)
-
New York
-
Rockland County New York (2)
-
Westchester County New York (1)
-
-
Newark Basin (49)
-
Pennsylvania
-
Berks County Pennsylvania (1)
-
Bucks County Pennsylvania (4)
-
Montgomery County Pennsylvania (3)
-
Northampton County Pennsylvania (1)
-
-
Reading Prong (2)
-
Reelfoot Rift (1)
-
Utah (1)
-
Virginia (1)
-
-
-
commodities
-
energy sources (5)
-
petroleum (2)
-
-
elements, isotopes
-
carbon
-
C-13/C-12 (1)
-
organic carbon (1)
-
-
isotope ratios (2)
-
isotopes
-
stable isotopes
-
C-13/C-12 (1)
-
O-18/O-16 (1)
-
-
-
metals
-
rare earths (1)
-
-
oxygen
-
O-18/O-16 (1)
-
-
-
fossils
-
Chordata
-
Vertebrata
-
Pisces
-
Osteichthyes
-
Actinopterygii (1)
-
-
-
Tetrapoda
-
Reptilia (1)
-
-
-
-
ichnofossils (1)
-
microfossils (1)
-
palynomorphs
-
miospores
-
pollen (1)
-
-
-
tracks (1)
-
-
geochronology methods
-
Ar/Ar (1)
-
fission-track dating (1)
-
K/Ar (1)
-
paleomagnetism (10)
-
-
geologic age
-
Mesozoic
-
Jurassic
-
Lower Jurassic
-
Feltville Formation (1)
-
Hampden Basalt (1)
-
Hettangian (3)
-
Holyoke Basalt (3)
-
lower Liassic (4)
-
Portland Formation (1)
-
Sinemurian (1)
-
Triassic-Jurassic boundary (1)
-
-
Middle Jurassic (1)
-
-
lower Mesozoic (5)
-
Newark Supergroup (16)
-
Passaic Formation (11)
-
Triassic
-
Upper Triassic
-
Carnian (2)
-
Chinle Formation (2)
-
Lockatong Formation (6)
-
Mercia Mudstone (2)
-
Norian (4)
-
Triassic-Jurassic boundary (1)
-
-
-
-
Paleozoic (1)
-
-
igneous rocks
-
igneous rocks
-
granophyre (1)
-
plutonic rocks
-
diabase (3)
-
-
volcanic rocks
-
basalts
-
tholeiite (2)
-
-
-
-
-
metamorphic rocks
-
metamorphic rocks
-
mylonites (1)
-
-
-
minerals
-
carbonates
-
aragonite (1)
-
calcite (1)
-
-
oxides (1)
-
phosphates
-
apatite (1)
-
-
silicates
-
framework silicates
-
silica minerals
-
quartz (1)
-
-
-
orthosilicates
-
nesosilicates
-
zircon group
-
zircon (1)
-
-
-
-
sheet silicates
-
chlorite group
-
chlorite (1)
-
-
clay minerals
-
smectite (1)
-
-
illite (1)
-
-
-
sulfates
-
gypsum (1)
-
-
-
Primary terms
-
absolute age (1)
-
Atlantic Ocean
-
North Atlantic
-
Gulf of Mexico (1)
-
Jeanne d'Arc Basin (1)
-
Northwest Atlantic (2)
-
-
-
Atlantic region (2)
-
atmosphere (1)
-
biogeography (2)
-
Canada
-
Eastern Canada
-
Maritime Provinces
-
Nova Scotia
-
Minas Basin (2)
-
-
-
-
-
carbon
-
C-13/C-12 (1)
-
organic carbon (1)
-
-
Chordata
-
Vertebrata
-
Pisces
-
Osteichthyes
-
Actinopterygii (1)
-
-
-
Tetrapoda
-
Reptilia (1)
-
-
-
-
clay mineralogy (1)
-
diagenesis (4)
-
earthquakes (1)
-
economic geology (5)
-
energy sources (5)
-
Europe
-
Southern Europe
-
Italy (1)
-
-
Western Europe
-
United Kingdom
-
Great Britain
-
England
-
Somerset England (2)
-
South-West England (2)
-
-
-
-
-
-
faults (10)
-
folds (4)
-
fractures (2)
-
geochemistry (8)
-
geochronology (6)
-
geophysical methods (4)
-
ground water (1)
-
heat flow (1)
-
ichnofossils (1)
-
igneous rocks
-
granophyre (1)
-
plutonic rocks
-
diabase (3)
-
-
volcanic rocks
-
basalts
-
tholeiite (2)
-
-
-
-
intrusions (3)
-
isotopes
-
stable isotopes
-
C-13/C-12 (1)
-
O-18/O-16 (1)
-
-
-
lava (6)
-
magmas (2)
-
Mesozoic
-
Jurassic
-
Lower Jurassic
-
Feltville Formation (1)
-
Hampden Basalt (1)
-
Hettangian (3)
-
Holyoke Basalt (3)
-
lower Liassic (4)
-
Portland Formation (1)
-
Sinemurian (1)
-
Triassic-Jurassic boundary (1)
-
-
Middle Jurassic (1)
-
-
lower Mesozoic (5)
-
Newark Supergroup (16)
-
Passaic Formation (11)
-
Triassic
-
Upper Triassic
-
Carnian (2)
-
Chinle Formation (2)
-
Lockatong Formation (6)
-
Mercia Mudstone (2)
-
Norian (4)
-
Triassic-Jurassic boundary (1)
-
-
-
-
metals
-
rare earths (1)
-
-
metamorphic rocks
-
mylonites (1)
-
-
metamorphism (1)
-
North America
-
Appalachian Basin (1)
-
Appalachians
-
Hudson Highlands (1)
-
-
Keweenawan Rift (1)
-
Michigan Basin (1)
-
-
oxygen
-
O-18/O-16 (1)
-
-
paleobotany (1)
-
paleoclimatology (4)
-
paleoecology (1)
-
paleogeography (5)
-
paleomagnetism (10)
-
paleontology (1)
-
Paleozoic (1)
-
palynomorphs
-
miospores
-
pollen (1)
-
-
-
petroleum (2)
-
petrology (1)
-
plate tectonics (1)
-
pollution (2)
-
reservoirs (1)
-
sedimentary rocks
-
carbonate rocks (1)
-
chemically precipitated rocks
-
evaporites (2)
-
-
clastic rocks
-
conglomerate (1)
-
mudstone (5)
-
red beds (4)
-
sandstone (4)
-
shale (5)
-
siltstone (1)
-
-
-
sedimentary structures
-
bedding plane irregularities
-
ripple marks (1)
-
-
planar bedding structures
-
cross-laminations (1)
-
laminations (1)
-
-
soft sediment deformation
-
clastic dikes (1)
-
-
-
sedimentation (4)
-
sediments (1)
-
seismology (1)
-
stratigraphy (12)
-
structural analysis (1)
-
structural geology (4)
-
tectonics
-
neotectonics (1)
-
salt tectonics (1)
-
-
underground installations (1)
-
United States
-
Arizona (1)
-
Arkoma Basin (1)
-
Atlantic Coastal Plain (6)
-
Connecticut
-
Hartford County Connecticut (2)
-
New Haven County Connecticut (3)
-
-
Culpeper Basin (5)
-
Dan River basin (1)
-
Eastern U.S. (13)
-
Florida
-
South Florida Basin (1)
-
-
Gettysburg Basin (1)
-
Great Smoky Mountains (1)
-
Hudson Valley (1)
-
Illinois Basin (1)
-
Kansas
-
Sedgwick Basin (1)
-
-
Kentucky
-
Rough Creek fault zone (1)
-
-
Massachusetts (2)
-
Mississippi Embayment (1)
-
Narragansett Basin (1)
-
New England (2)
-
New Jersey
-
Hunterdon County New Jersey (1)
-
Mercer County New Jersey (2)
-
Middlesex County New Jersey (1)
-
Morris County New Jersey (4)
-
Somerset County New Jersey (3)
-
Warren County New Jersey (1)
-
Watchung Mountains (1)
-
-
New Mexico (1)
-
New York
-
Rockland County New York (2)
-
Westchester County New York (1)
-
-
Newark Basin (49)
-
Pennsylvania
-
Berks County Pennsylvania (1)
-
Bucks County Pennsylvania (4)
-
Montgomery County Pennsylvania (3)
-
Northampton County Pennsylvania (1)
-
-
Reading Prong (2)
-
Reelfoot Rift (1)
-
Utah (1)
-
Virginia (1)
-
-
weathering (1)
-
-
rock formations
-
Stockton Formation (1)
-
-
sedimentary rocks
-
sedimentary rocks
-
carbonate rocks (1)
-
chemically precipitated rocks
-
evaporites (2)
-
-
clastic rocks
-
conglomerate (1)
-
mudstone (5)
-
red beds (4)
-
sandstone (4)
-
shale (5)
-
siltstone (1)
-
-
-
siliciclastics (1)
-
-
sedimentary structures
-
sedimentary structures
-
bedding plane irregularities
-
ripple marks (1)
-
-
planar bedding structures
-
cross-laminations (1)
-
laminations (1)
-
-
soft sediment deformation
-
clastic dikes (1)
-
-
-
tracks (1)
-
-
sediments
-
sediments (1)
-
siliciclastics (1)
-
-
soils
-
paleosols (1)
-
Newark Basin
The “Passive” Margin of Eastern North America: Rifting and the Influence of Prerift Orogenic Activity on Postrift Development
Reservoir and sealing properties of the Newark rift basin formations: Implications for carbon sequestration
A tight coupling between atmospheric p CO 2 and sea-surface temperature in the Late Triassic
Abstract Limited exploratory drilling based on relatively sparse seismic data has occurred since at least 1890 in onshore Late Triassic–Early Jurassic rift basins of the eastern United States (U.S.). Although rich source rocks and thermally generated hydrocarbons have been documented, commercial petroleum accumulations have not been found. Consequently, in 2012 the U.S. Geological Survey (USGS) assessed these basins as having potentially modest volumes of primarily continuous (unconventional) resources. Using these findings and interpretations, what then is the prospectivity of similar age undrilled rift basins in the offshore of the U.S. Central Atlantic? Are there any indications of differences between the offshore and onshore basins in the apparent mode of formation, structural style, amount of inversion, etc. , documented, or suggested by seismic data in these undrilled offshore basins? What do we know, and what can we speculate regarding petroleum system elements and processes in these unexplored basins? Seismic data interpretation suggests most offshore rift basins are generally similar to the Late Triassic–Early Jurassic rift basins onshore. The amount of eroded synrift strata predicted by geohistory modeling in the seismically defined Norfolk basin, offshore Virginia, is similar to that of onshore basins. However, seismic data interpretation also shows differences among some of the offshore basins; e.g. , a rift system northwest of the Yarmouth arch in the northern Georges Bank basin, offshore New England, appears to have less synrift section eroded than most basins in the U.S. Central Atlantic and contains inversion features that appear seismically similar to productive structures found offshore Indonesia.
A 30 Myr record of Late Triassic atmospheric p CO 2 variation reflects a fundamental control of the carbon cycle by changes in continental weathering
Overview of the Origin, Depositional Histories, and Petroleum Systems of the Sedimentary Basins of the Eastern United States
Abstract Sedimentary basins in the eastern United States (U.S.) contain strata ranging in age from Neoproterozoic to Holocene and have been the source of petroleum and coal that fueled much of the initial growth and development of the U.S. as a major industrial power. It is estimated that at least 87 billion barrels of oil (BBO) and natural gas liquids (BBNGL) and 664 trillion cubic feet of natural gas (TCFG) have been produced to-date from these basins. These basins developed on continental and transitional oceanic-continental crust ranging in age from the Paleoproterozoic to Triassic. Many of these basins have undergone structural readjustment and uplift, some being nearly completely inverted. The oldest of these basins considered here are Mesoproterozoic to Early Cambrian in age. They include the Midcontinent rift, Reelfoot rift, Rough Creek graben, and Rome trough. These basins are dominantly rift basins, which formed within the North American craton, presumably as a result of plate tectonic forces associated with the rifting of the Rodina supercontinent and the opening of the Iapetus Ocean. Petroleum systems have been identified or postulated in these four basins. Overlying these basins are the three large Paleozoic-aged sag-foreland basins of the eastern U.S.: the Michigan, Illinois, and Appalachian basins. Additionally included are the eastern extent of the Arkoma-Ouachita-Black Warrior foreland basin and a relict Gondwanan basin that was left behind in present-day north Florida following the Mesozoic rifting of Pangea. A mixed siliciclastic–carbonate–evaporite sedimentary section includes reservoirs and seal facies for many play types. Multiple petroleum systems have been identified or postulated in all of these basins. Succeeding these large Paleozoic sag and foreland basins are the Late Permian(?) to Early Jurassic rift basins that rim the eastern continental margin of the U.S. These basins have formed as a result of plate tectonic forces associated with the opening of the Atlantic Ocean and the Gulf of Mexico. Basin-fill sequences are generally lacustrine and continental-playa siliciclastic strata containing locally significant coals and minor carbonates. Petroleum systems have been identified or postulated in several of these basins, including the Dan River-Danville, Deep River, Newark, Richmond, and Taylorsville basins. Finally, overlying this complex stack of Proterozoic, Paleozoic, and early Mesozoic basins are the great Gulf of Mexico and Atlantic margin basins. The Gulf of Mexico Basin is distinguished by the dominating structural control of the salt and shale tectonics on a mobile substrate, whereas the basins of the western Atlantic margin are associated mainly with faulting associated with the opening of the Atlantic Ocean. Only the Carolina Trough of the western Atlantic margin basins has mobile salt structures. The sedimentary sequences of both basins are a mixed siliciclastic–carbonate interval containing coal and lignite in variable quantities in the updip portions of the basins. A composite total petroleum system has been identified in the Gulf of Mexico basin that incorporates several Mesozoic and Cenozoic petroleum source rocks with many reservoir rocks and seals throughout the sedimentary sequence. A combination of cultural and tectonic setting, sediment provenance and delivery systems, and paleo-oceanographic conditions have made the Gulf of Mexico basin one of the most prolific petroleum provinces on the planet. The current understanding of the Atlantic margin basin suggests that it does not appear to have a similar accumulation of petroleum resources as the Gulf of Mexico Basin. Correlated and potential petroleum source rock intervals have been penetrated in several of the offshore post-rift Atlantic margin subbasins; however, in many places on the shallow shelf, these intervals are generally too organically lean and (or) too immature to be major source rocks. A single petroleum system has been locally demonstrated in the offshore Atlantic by a non-commercial gas-condensate discovery. Additional petroleum systems in the western Atlantic may be identified as research continues. Source rock intervals penetrated by Deep Sea Drilling Project and Ocean Drilling Program cruises farther off-shore have generative potential, but data from these projects are too sparse to identify petroleum systems connecting these source rocks with potential reservoir targets.