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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Paleozoic
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Middle Permian (1)
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Cadeby Formation (3)
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Zechstein (146)
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Werra Series (2)
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Precambrian
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Primary terms
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Asia
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Atlantic Ocean
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Cenozoic
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Pliocene
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Chordata
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Vertebrata
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N-15/N-14 (1)
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mantle (1)
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Mesozoic
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Cretaceous
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Lower Cretaceous
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Upper Cretaceous
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Cenomanian (1)
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Maestrichtian (1)
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Turonian (1)
-
-
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Jurassic
-
Heather Formation (1)
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Lower Jurassic
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Toarcian
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lower Toarcian (1)
-
-
-
Middle Jurassic
-
Callovian (2)
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Dogger (1)
-
-
Posidonia Shale (1)
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Upper Jurassic
-
Fulmar Formation (3)
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Kimmeridge Clay (3)
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Kimmeridgian
-
lower Kimmeridgian (1)
-
upper Kimmeridgian (1)
-
-
Oxfordian (2)
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Volgian (2)
-
-
-
Statfjord Formation (1)
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Triassic
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Lower Triassic
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Bunter (9)
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Permian-Triassic boundary (1)
-
-
Middle Triassic
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Anisian (1)
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Ladinian (1)
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Muschelkalk (1)
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Sherwood Sandstone (2)
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Upper Triassic
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Carnian (1)
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Keuper (2)
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Mercia Mudstone (1)
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Norian (1)
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Rhaetian
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Penarth Group (1)
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metal ores
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iron ores (1)
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metals
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sodium (1)
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alkaline earth metals
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Sr-87/Sr-86 (1)
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copper (2)
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gold (1)
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platinum group
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rare earths
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ocean floors (1)
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Paleozoic
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Devonian
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Upper Devonian (1)
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Permian
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Guadalupian (2)
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Lower Permian
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Leman Sandstone Formation (3)
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Middle Permian (1)
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Rotliegendes (34)
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Upper Permian
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Cadeby Formation (3)
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Lopingian (6)
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Permian-Triassic boundary (1)
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Zechstein (146)
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Werra Series (2)
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-
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palynology (1)
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palynomorphs
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miospores
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pollen (1)
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paragenesis (1)
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petroleum
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natural gas (23)
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petrology (1)
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phase equilibria (3)
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Plantae
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Spermatophyta
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Gymnospermae (1)
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plate tectonics (7)
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potash (4)
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upper Precambrian
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Proterozoic
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Paleoproterozoic (1)
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remote sensing (1)
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sea-level changes (7)
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sedimentary petrology (2)
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sedimentary rocks
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chalk (5)
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dolostone (3)
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packstone (1)
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chemically precipitated rocks
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evaporites
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salt (14)
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clastic rocks
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black shale (1)
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marl (1)
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mudstone (4)
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red beds (1)
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sedimentary structures
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stratigraphy (11)
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S-34/S-32 (1)
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tectonics
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Texas
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chemically precipitated rocks
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salt (14)
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clastic rocks
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black shale (1)
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marl (1)
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mudstone (4)
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red beds (1)
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shale (2)
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sedimentary structures
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Zechstein
The influence of salt tectonics on the distribution of the Triassic Skagerrak Formation in the Ula Field, Norwegian North Sea
Regional variability of onset and cessation of salt tectonics in the Mesozoic and Cenozoic Southern North Sea subbasins
Three-dimensional seismic classification of salt structure morphologies across the Southern North Sea
Gravity imaging of sub-Zechstein geological structures in the UK sector of the North Sea using the gravity layer stripping method
Diagenetic History and Timing of Cu and Zn-Pb Sulfide Mineralization in the Permian Kupferschiefer System, Saale Subbasin, Eastern Germany
Use of exploration methods to repurpose and extend the life of a super basin as a carbon storage hub for the energy transition
Late Permian evaporite facies variation in the Forth Approaches Basin, North Sea: implications for hydrogen storage
Rebuilding the foundation of late Paleozoic pinnid bivalve study (family Pinnidae)
Geological evaluation of suprasalt carbon storage opportunities in the Silverpit Basin, United Kingdom Southern North Sea
The Hampole Discontinuity and Hampole Beds (Cadeby Formation, Upper Permian): deposition on the Zechstein English Shelf, South Yorkshire, UK, with data from new exposures
FIRST REPORT OF FUNGAL PALYNOMORPHS FROM THE ZECHSTEIN GROUP (LOPINGIAN): IMPLICATIONS FOR THE STRATIGRAPHIC COMPLETENESS OF THE EARTH'S PALEOZOIC FUNGAL RECORD
The role of the underburden at Elgin Franklin in the understanding of the overburden 4D signal
Geology of the Johan Sverdrup field: A giant oil discovery and development project in a mature Norwegian North Sea basin
Estimating subsurface properties using a semisupervised neural network approach
Origin, migration pathways, and prediction of high carbon dioxide accumulations in the Lower Saxony Basin (northwestern Germany): Part I
Origin, migration pathways, and prediction of high carbon dioxide accumulations in the Lower Saxony Basin (northwestern Germany): Part II
Evaporite palynology: a case study of the Permian (Lopingian) Zechstein Sea
A possible serpulid tube worm of the genus Filograna from the upper Permian Cadeby Formation of South Yorkshire, UK
The Vale of Pickering gas fields: Kirby Misperton, Malton, Marishes and Pickering, North Yorkshire, UK Onshore
Abstract The Vale of Pickering gas fields were discovered over a 20-year period. The development scheme was aimed to deliver 9.3 MMscfd gas to the Knapton Power Station nearby. Cumulative production is 30.3 bcf from an estimated 172 bcf gas initially in place. The gas fields comprise a series of low relief structures at depths around 5000 ft true depth subsea. The primary reservoir is Zechstein Group dolomitized and fractured carbonates of the Permian Kirkham Abbey Formation with average reservoir quality ranges of 12–13% porosity and 0.5–1.5 mD permeability. Secondary reservoirs exist in Carboniferous sandstones directly below the Base Permian Unconformity. The gas is sourced from Lower Carboniferous shales. The fields were discovered using 2D seismic data and subsequent 3D seismic data have been merged to form a 260 km 2 dataset. Zechstein production has been limited by early water breakthrough. Artificial lift is planned to enhance the gas flow rate on the Pickering Field and anticipated water influx will be re-injected. If this enhanced gas recovery scheme is successful it can be applied to the other fields. Plans to hydraulically fracture a number of zones in the Carboniferous Lower Bowland Section are in progress.
Abstract The abandoned Juliet gas field is a small, highly compartmentalized, accumulation situated south and east of the Amethyst Gas Field. It was discovered in 2008 by well 47/14b-10 and flowed first gas on 5 January 2014. The field consists of at least two culminations within a very low-relief east–west-orientated fault-bounded anticline. The reservoir comprises aeolian sandstones of the Permian, Rotliegend Group, Leman Sandstone Formation. Reservoir quality varies from good to moderate, with a high production rate achieved from horizontal wells. Seismic time-to-depth conversion is affected by Quaternary seabed channels, chalk burial history and a rapid thickening in the Basalanhydrit Formation located over the east of the field, associated with the edge of the Zechstein Basin. Gas-in-place at pre-development was expected to be 105 bcf, with reserves of 67 bcf. The field was developed using two horizontal wells and a subsea tie-back to the Pickerill Field, 22 km to the east. Since development, the field appears to be more compartmentalized than initially expected.