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NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
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Africa
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Central Africa
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Angola
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Cuanza Basin (1)
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North Africa
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Egypt
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Sinai Egypt (1)
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Morocco
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Taourirt Morocco (1)
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Southern Africa
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Arctic Ocean
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Barents Sea (2)
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Arctic region
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Svalbard
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Asia
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Taiwan
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Atlantic Ocean
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Murmansk Russian Federation
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East Pacific Ocean Islands
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Pacific Ocean
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North Pacific
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elements, isotopes
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stable isotopes
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Pb-208 (1)
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metals
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uranium
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lead
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oxygen
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fossils
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Chordata
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Vertebrata
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Mammalia (1)
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Reptilia
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Diapsida
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Archosauria
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dinosaurs (1)
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Invertebrata
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Arthropoda
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Brachiopoda (1)
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microfossils
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Plantae
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Chlorophyta
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geochronology methods
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geologic age
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Tertiary
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Neogene
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middle Miocene
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upper Miocene
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Pliocene (3)
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Paleogene
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Eocene
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lower Eocene
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middle Eocene
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Mirador Formation (1)
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Oligocene (6)
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Tulare Formation (1)
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upper Cenozoic (1)
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Dakota Formation (1)
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Mancos Shale (1)
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Cody Shale (1)
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Frontier Formation (1)
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Javelina Formation (2)
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Niobrara Formation (2)
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Franciscan Complex (1)
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Arapien Shale (1)
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Bowser Lake Group (1)
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Morrison Formation (2)
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Sundance Formation (2)
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Navajo Sandstone (1)
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Triassic
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Upper Triassic
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Yanchang Formation (2)
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Yanshanian (2)
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Paleozoic
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Carboniferous
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Mississippian (2)
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Devonian
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Middle Devonian
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Onondaga Limestone (1)
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Matapedia Group (1)
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Ordovician
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Middle Ordovician (2)
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Trenton Group (2)
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Upper Ordovician
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Caradocian (1)
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Trentonian (2)
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Permian (4)
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Silurian
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Lower Silurian
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Tuscarora Formation (1)
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Upper Silurian (1)
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Tensleep Sandstone (1)
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upper Paleozoic (3)
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Phanerozoic (1)
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Precambrian
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Archean
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Gilman Formation (1)
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Chuar Group (1)
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Unkar Group (2)
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upper Precambrian
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Proterozoic
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Mesoproterozoic (2)
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Neoproterozoic
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Riphean (1)
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Vendian (1)
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Paleoproterozoic (1)
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igneous rocks
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extrusive rocks (1)
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igneous rocks
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granophyre (1)
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plutonic rocks
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granites (2)
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granodiorites (1)
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ultramafics
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volcanic rocks
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basalts
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flood basalts (1)
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pyroclastics (1)
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ophiolite (1)
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metamorphic rocks
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metamorphic rocks
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ophiolite (1)
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minerals
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minerals (1)
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phosphates
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apatite (1)
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silicates
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framework silicates
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alkali feldspar
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K-feldspar (1)
-
-
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orthosilicates
-
nesosilicates
-
zircon group
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zircon (3)
-
-
-
-
-
sulfides
-
arsenopyrite (1)
-
-
-
Primary terms
-
absolute age (7)
-
Africa
-
Central Africa
-
Angola
-
Cuanza Basin (1)
-
-
-
North Africa
-
Egypt
-
Sinai Egypt (1)
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Morocco
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Taourirt Morocco (1)
-
-
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Southern Africa
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South Africa
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Bushveld Complex (1)
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Merensky Reef (1)
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Transvaal region (1)
-
-
-
-
Arctic Ocean
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Barents Sea (2)
-
-
Arctic region
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Greenland
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Northern Greenland (1)
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Svalbard
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Spitsbergen
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Spitsbergen Island (1)
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-
-
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Asia
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Far East
-
China
-
North China Platform (1)
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Ordos Basin (2)
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Qaidam Basin (1)
-
Qinghai China (1)
-
-
Taiwan
-
Chelungpu Fault (1)
-
-
-
Kamchatka Russian Federation
-
Kamchatka Peninsula
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Tolbachik (1)
-
-
-
Russian Pacific region (1)
-
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Atlantic Ocean
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North Atlantic
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South Atlantic
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Canada
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Ontario
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Quebec
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carbon
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C-13/C-12 (2)
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C-14 (1)
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Caribbean region
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West Indies
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Antilles
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Lesser Antilles
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Antigua (1)
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-
-
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Cenozoic
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Quaternary
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Geomechanical Modeling of Ground Surface Deformation Associated with Thrust and Reverse‐Fault Earthquakes: A Distinct Element Approach
Shallow deformation on the Kirby Hills fault, Sacramento–San Joaquin Delta, California (USA), revealed from high-resolution seismic reflection data and coring in a fluvial system
Analogue modeling of domino-style extensional basement fault systems with prekinematic salt
The Cretaceous-Paleogene contact in the Tornillo Group of Big Bend National Park, West Texas, USA
Shallow Faulting and Folding in the Epicentral Area of the 1886 Charleston, South Carolina, Earthquake
Abstract The Carrack Field, located in the Southern North Sea Blocks 49/14b and 49/15a, has of the order or 15 bcm (530 bcf) gas initially in place and is operated by Shell UK Ltd. The field consists of a pop-up structure in the south of the field and extends to the north with a gently-dipping monoclinal structure. The reservoir comprises sandstones of the Permian Silverpit and Leman Sandstone formations, which contain c. 85% of the in-place resources. The quality of the reservoir decreases rapidly to the north. Gas is also produced from Carboniferous sandstones of late Duckmantian (Westphalian B)–Bolsovian (Westphalian C) age. Initially, the field was in pressure communication both laterally and vertically with a single gas–water contact. During production time, however, the three main fault blocks behaved independently, and decimetre-thick shale intervals acted as vertical baffles between the sandstone units. The Carrack Field has been in production since 2003 and is developed by a single platform with seven mainly deviated wells. The current production rate is c. 0.7 MMm 3 /day (25 MMscfgd). Until the end of field life in the 2030s, the field is expected to produce gas of the order of a few bcm. The main remaining opportunity is the undeveloped Carrack West compartment.