FORMATION MEMBER STAGE ZONE
The lower part of the Kap Stewart Formation, formed by the domi-nantly conglomeratic 'barren sandstone', represents alluvial fan de-posits. Upwards there is a marked change to the well developed fining upwards sequences of the 'plant-bearing series ' which com-prise three facies:...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.549.7547 2023-05-15T16:03:41+02:00 FORMATION MEMBER STAGE ZONE Jameson Land East Greenland Richard M. Sykes I. Fluviatile Kap Stewart Formation Department Of Geology Neill Klinter Fleming Fjord Gule Horn The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.7547 http://2dgf.dk/xpdf/bull23-03-04-203-212.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.7547 http://2dgf.dk/xpdf/bull23-03-04-203-212.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://2dgf.dk/xpdf/bull23-03-04-203-212.pdf text ftciteseerx 2016-01-08T11:27:29Z The lower part of the Kap Stewart Formation, formed by the domi-nantly conglomeratic 'barren sandstone', represents alluvial fan de-posits. Upwards there is a marked change to the well developed fining upwards sequences of the 'plant-bearing series ' which com-prise three facies: 1. Coarse arkosic sandstones and conglomerates; 2. Fine rippled bioturbated green sandstones; 3.Variegated siltstones with plant remains and occasional rootlet beds and coal seams. Trough shaped channels, unidirectional palaeocurrents and a lack of epsilon cross-beds all indicate a low sinuosity non braided river environment in close proximity to a SSE source area. In the basal Jurassic a humid climate coal belt in Northern Europe and East Greenland contrasts with an arid climate evaporite belt in Morocco Text East Greenland Greenland Unknown Greenland Kap ENVELOPE(23.567,23.567,65.533,65.533) Kap Stewart ENVELOPE(-22.633,-22.633,70.433,70.433) |
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Open Polar |
collection |
Unknown |
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ftciteseerx |
language |
English |
description |
The lower part of the Kap Stewart Formation, formed by the domi-nantly conglomeratic 'barren sandstone', represents alluvial fan de-posits. Upwards there is a marked change to the well developed fining upwards sequences of the 'plant-bearing series ' which com-prise three facies: 1. Coarse arkosic sandstones and conglomerates; 2. Fine rippled bioturbated green sandstones; 3.Variegated siltstones with plant remains and occasional rootlet beds and coal seams. Trough shaped channels, unidirectional palaeocurrents and a lack of epsilon cross-beds all indicate a low sinuosity non braided river environment in close proximity to a SSE source area. In the basal Jurassic a humid climate coal belt in Northern Europe and East Greenland contrasts with an arid climate evaporite belt in Morocco |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Jameson Land East Greenland Richard M. Sykes I. Fluviatile Kap Stewart Formation Department Of Geology Neill Klinter Fleming Fjord Gule Horn |
spellingShingle |
Jameson Land East Greenland Richard M. Sykes I. Fluviatile Kap Stewart Formation Department Of Geology Neill Klinter Fleming Fjord Gule Horn FORMATION MEMBER STAGE ZONE |
author_facet |
Jameson Land East Greenland Richard M. Sykes I. Fluviatile Kap Stewart Formation Department Of Geology Neill Klinter Fleming Fjord Gule Horn |
author_sort |
Jameson Land |
title |
FORMATION MEMBER STAGE ZONE |
title_short |
FORMATION MEMBER STAGE ZONE |
title_full |
FORMATION MEMBER STAGE ZONE |
title_fullStr |
FORMATION MEMBER STAGE ZONE |
title_full_unstemmed |
FORMATION MEMBER STAGE ZONE |
title_sort |
formation member stage zone |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.7547 http://2dgf.dk/xpdf/bull23-03-04-203-212.pdf |
long_lat |
ENVELOPE(23.567,23.567,65.533,65.533) ENVELOPE(-22.633,-22.633,70.433,70.433) |
geographic |
Greenland Kap Kap Stewart |
geographic_facet |
Greenland Kap Kap Stewart |
genre |
East Greenland Greenland |
genre_facet |
East Greenland Greenland |
op_source |
http://2dgf.dk/xpdf/bull23-03-04-203-212.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.7547 http://2dgf.dk/xpdf/bull23-03-04-203-212.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766399386531659776 |