Development of the Lower Cambrian-Middle Ordovician Carbonate Platform: North Atlantic Region

Publikation: Bidrag til bog/antologi/rapport › Bidrag til bog/antologi › Forskning › fagfællebedømt

Standard

Development of the Lower Cambrian-Middle Ordovician Carbonate Platform: North Atlantic Region. / Stouge, Svend; Harper, David A.T.; Boyce, William D. ; Knight, Ian; Christiansen, Jørgen L.

The great American carbonate bank: The geology and economic resources of the Cambrian - Ordovician Sauk megasequence of Laurentia. red. / J.R. Derby; R.D. Fritz; S.A. Longacre; W.A. Morgan; C.A. Sternbach. Bind 98 AAPG Memoir, 2012. s. 597-626.

Publikation: Bidrag til bog/antologi/rapport › Bidrag til bog/antologi › Forskning › fagfællebedømt

Harvard

Stouge, S, Harper, DAT, Boyce, WD, Knight, I & Christiansen, JL 2012, Development of the Lower Cambrian-Middle Ordovician Carbonate Platform: North Atlantic Region. i JR Derby, RD Fritz, SA Longacre, WA Morgan & CA Sternbach (red), The great American carbonate bank: The geology and economic resources of the Cambrian - Ordovician Sauk megasequence of Laurentia. bind 98, AAPG Memoir, s. 597-626. https://doi.org/DOI:10.1306/13331509M983508

APA

Stouge, S., Harper, D. A. T., Boyce, W. D., Knight, I., & Christiansen, J. L. (2012). Development of the Lower Cambrian-Middle Ordovician Carbonate Platform: North Atlantic Region. I J. R. Derby, R. D. Fritz, S. A. Longacre, W. A. Morgan, & C. A. Sternbach (red.), The great American carbonate bank: The geology and economic resources of the Cambrian - Ordovician Sauk megasequence of Laurentia (Bind 98, s. 597-626). AAPG Memoir. https://doi.org/DOI:10.1306/13331509M983508

Vancouver

Stouge S, Harper DAT, Boyce WD, Knight I, Christiansen JL. Development of the Lower Cambrian-Middle Ordovician Carbonate Platform: North Atlantic Region. I Derby JR, Fritz RD, Longacre SA, Morgan WA, Sternbach CA, red., The great American carbonate bank: The geology and economic resources of the Cambrian - Ordovician Sauk megasequence of Laurentia. Bind 98. AAPG Memoir. 2012. s. 597-626 https://doi.org/DOI:10.1306/13331509M983508

Author

Stouge, Svend ; Harper, David A.T. ; Boyce, William D. ; Knight, Ian ; Christiansen, Jørgen L. / Development of the Lower Cambrian-Middle Ordovician Carbonate Platform: North Atlantic Region. The great American carbonate bank: The geology and economic resources of the Cambrian - Ordovician Sauk megasequence of Laurentia. red. / J.R. Derby ; R.D. Fritz ; S.A. Longacre ; W.A. Morgan ; C.A. Sternbach. Bind 98 AAPG Memoir, 2012. s. 597-626

Bibtex

@inbook{b9c6e79ca1854293ba49a765753de343,
title = "Development of the Lower Cambrian-Middle Ordovician Carbonate Platform: North Atlantic Region",
abstract = "The northeastern margin of Laurentia formed an important part of the Iapetus Ocean and includes the development of the Franklinian Basin in North Greenland and Arctic Canada. The uninterrupted continental margin bordering the North American craton is represented by well-exposed successions in Northeast and eastern North Greenland, together with Svalbard and Bj{\o}rn{\o}ya. Physiographically, the northeastern margin of Laurentia during the early Paleozoic history of Greenland was a northward extension of the passive rifted continentalmargin of the Caledonian continental edge of Laurentia. It was a transform-rifted margin and represents the part of the Laurentian margin that borders the Arctic part of the North Atlantic Ocean. Geologically, the northwestern segment of the continental margin has a somewhat different setting and development from farther south in the Northeast Greenland–Svalbard segment but both regions overlie a thick and extensive package of Neoproterozoic rocks andwere affected by the Caledonian orogeny.",
keywords = "Faculty of Science, Cambrium, Ordovician, Carbonate Platform, Laurentia, Nort Atlantic Region, Greenland, Svalbard archipelago (Norway)",
author = "Svend Stouge and Harper, {David A.T.} and Boyce, {William D.} and Ian Knight and Christiansen, {J{\o}rgen L.}",
year = "2012",
doi = "DOI:10.1306/13331509M983508",
language = "English",
volume = "98",
pages = "597--626",
editor = "J.R. Derby and R.D. Fritz and S.A. Longacre and Morgan, {W.A. } and C.A. Sternbach",
booktitle = "The great American carbonate bank: The geology and economic resources of the Cambrian - Ordovician Sauk megasequence of Laurentia",
publisher = "AAPG Memoir",

}

RIS

TY - CHAP

T1 - Development of the Lower Cambrian-Middle Ordovician Carbonate Platform: North Atlantic Region

AU - Stouge, Svend

AU - Harper, David A.T.

AU - Boyce, William D.

AU - Knight, Ian

AU - Christiansen, Jørgen L.

PY - 2012

Y1 - 2012

N2 - The northeastern margin of Laurentia formed an important part of the Iapetus Ocean and includes the development of the Franklinian Basin in North Greenland and Arctic Canada. The uninterrupted continental margin bordering the North American craton is represented by well-exposed successions in Northeast and eastern North Greenland, together with Svalbard and Bjørnøya. Physiographically, the northeastern margin of Laurentia during the early Paleozoic history of Greenland was a northward extension of the passive rifted continentalmargin of the Caledonian continental edge of Laurentia. It was a transform-rifted margin and represents the part of the Laurentian margin that borders the Arctic part of the North Atlantic Ocean. Geologically, the northwestern segment of the continental margin has a somewhat different setting and development from farther south in the Northeast Greenland–Svalbard segment but both regions overlie a thick and extensive package of Neoproterozoic rocks andwere affected by the Caledonian orogeny.

AB - The northeastern margin of Laurentia formed an important part of the Iapetus Ocean and includes the development of the Franklinian Basin in North Greenland and Arctic Canada. The uninterrupted continental margin bordering the North American craton is represented by well-exposed successions in Northeast and eastern North Greenland, together with Svalbard and Bjørnøya. Physiographically, the northeastern margin of Laurentia during the early Paleozoic history of Greenland was a northward extension of the passive rifted continentalmargin of the Caledonian continental edge of Laurentia. It was a transform-rifted margin and represents the part of the Laurentian margin that borders the Arctic part of the North Atlantic Ocean. Geologically, the northwestern segment of the continental margin has a somewhat different setting and development from farther south in the Northeast Greenland–Svalbard segment but both regions overlie a thick and extensive package of Neoproterozoic rocks andwere affected by the Caledonian orogeny.

KW - Faculty of Science

KW - Cambrium

KW - Ordovician

KW - Carbonate Platform

KW - Laurentia

KW - Nort Atlantic Region

KW - Greenland

KW - Svalbard archipelago (Norway)

U2 - DOI:10.1306/13331509M983508

DO - DOI:10.1306/13331509M983508

M3 - Book chapter

VL - 98

SP - 597

EP - 626

BT - The great American carbonate bank: The geology and economic resources of the Cambrian - Ordovician Sauk megasequence of Laurentia

A2 - Derby, J.R.

A2 - Fritz, R.D.

A2 - Longacre, S.A.

A2 - Morgan, W.A.

A2 - Sternbach, C.A.

PB - AAPG Memoir

ER -

ID: 231901288