Diagenesis and porosity evolution of Lower Permian Palaeoaplysina buildups, Bjornoya, Barents Sea: an example of diagenetic response to high frequency sea level fluctuations in an arid climate

L. Stemmerik; G. B. Larssen

Diagenesis and porosity evolution of Lower Permian Palaeoaplysina buildups, Bjornoya, Barents Sea: an example of diagenetic response to high frequency sea level fluctuations in an arid climate

L. Stemmerik, G. B. Larssen

Afdeling for Geoenergi og -lagring

Publikation: Bidrag til bog/rapport/konferenceproceedings › Bogkapitel › Forskning › peer review

27 Citationer (Scopus)

Abstrakt

The lower Kapp Duner Formation on Bjornoya consists of two Palaeoaplysina bukldup complexes separated by a karst surfce, believed to represent a third order sequence boundary. The buildup complexes are composed of 3-10 m-thick, stacked, shallowing upward cycles of restricted shelf wackestone and Palaeoaplysina wackestone and packstone. Each cycle is terminated by an event of subaerial exposure related to fourth order fluctuations in sea level. -from Authors

Originalsprog	Engelsk
Titel	Diagenesis and Basin Development
Redaktører	Andrew D. Horbury, Andrew G. Robinson
Forlag	American Association of Petroleum Geologists
Sider	199-211
Antal sider	13
Vol/bind	Studies in Geology 36
Status	Udgivet - 1993

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Stemmerik, L., & Larssen, G. B. (1993). Diagenesis and porosity evolution of Lower Permian Palaeoaplysina buildups, Bjornoya, Barents Sea: an example of diagenetic response to high frequency sea level fluctuations in an arid climate. I A. D. Horbury, & A. G. Robinson (red.), Diagenesis and Basin Development (Bind Studies in Geology 36, s. 199-211). American Association of Petroleum Geologists.

Stemmerik, L. ; Larssen, G. B. / Diagenesis and porosity evolution of Lower Permian Palaeoaplysina buildups, Bjornoya, Barents Sea : an example of diagenetic response to high frequency sea level fluctuations in an arid climate. Diagenesis and Basin Development. red. / Andrew D. Horbury ; Andrew G. Robinson. Bind Studies in Geology 36 American Association of Petroleum Geologists, 1993. s. 199-211

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title = "Diagenesis and porosity evolution of Lower Permian Palaeoaplysina buildups, Bjornoya, Barents Sea: an example of diagenetic response to high frequency sea level fluctuations in an arid climate",

abstract = "The lower Kapp Duner Formation on Bjornoya consists of two Palaeoaplysina bukldup complexes separated by a karst surfce, believed to represent a third order sequence boundary. The buildup complexes are composed of 3-10 m-thick, stacked, shallowing upward cycles of restricted shelf wackestone and Palaeoaplysina wackestone and packstone. Each cycle is terminated by an event of subaerial exposure related to fourth order fluctuations in sea level. -from Authors",

author = "L. Stemmerik and Larssen, {G. B.}",

year = "1993",

language = "English",

volume = "Studies in Geology 36",

pages = "199--211",

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Stemmerik, L & Larssen, GB 1993, Diagenesis and porosity evolution of Lower Permian Palaeoaplysina buildups, Bjornoya, Barents Sea: an example of diagenetic response to high frequency sea level fluctuations in an arid climate. i AD Horbury & AG Robinson (red), Diagenesis and Basin Development. bind Studies in Geology 36, American Association of Petroleum Geologists, s. 199-211.

Diagenesis and porosity evolution of Lower Permian Palaeoaplysina buildups, Bjornoya, Barents Sea : an example of diagenetic response to high frequency sea level fluctuations in an arid climate. / Stemmerik, L.; Larssen, G. B.

Diagenesis and Basin Development. red. / Andrew D. Horbury; Andrew G. Robinson. Bind Studies in Geology 36 American Association of Petroleum Geologists, 1993. s. 199-211.

Publikation: Bidrag til bog/rapport/konferenceproceedings › Bogkapitel › Forskning › peer review

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N2 - The lower Kapp Duner Formation on Bjornoya consists of two Palaeoaplysina bukldup complexes separated by a karst surfce, believed to represent a third order sequence boundary. The buildup complexes are composed of 3-10 m-thick, stacked, shallowing upward cycles of restricted shelf wackestone and Palaeoaplysina wackestone and packstone. Each cycle is terminated by an event of subaerial exposure related to fourth order fluctuations in sea level. -from Authors

AB - The lower Kapp Duner Formation on Bjornoya consists of two Palaeoaplysina bukldup complexes separated by a karst surfce, believed to represent a third order sequence boundary. The buildup complexes are composed of 3-10 m-thick, stacked, shallowing upward cycles of restricted shelf wackestone and Palaeoaplysina wackestone and packstone. Each cycle is terminated by an event of subaerial exposure related to fourth order fluctuations in sea level. -from Authors

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Stemmerik L, Larssen GB. Diagenesis and porosity evolution of Lower Permian Palaeoaplysina buildups, Bjornoya, Barents Sea: an example of diagenetic response to high frequency sea level fluctuations in an arid climate. I Horbury AD, Robinson AG, red., Diagenesis and Basin Development. Bind Studies in Geology 36. American Association of Petroleum Geologists. 1993. s. 199-211

Diagenesis and porosity evolution of Lower Permian Palaeoaplysina buildups, Bjornoya, Barents Sea: an example of diagenetic response to high frequency sea level fluctuations in an arid climate

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