DOI: 10.1306/12031212093
Scopus记录号: 2-s2.0-84879530494
论文题名: Permian-hobcene tectonostratigraphic evolution of the Mandal high, central graben, North Sea
作者: Rossland A. ; Escalona A. ; Rolfsen R.
刊名: AAPG Bulletin
ISSN: 0149-1676
EISSN: 1558-9406
出版年: 2013
发表日期: 2013
卷: 97, 期: 6 起始页码: 923
结束页码: 957
语种: 英语
Scopus关键词: Continental environments
; Continental rifting
; Early Cretaceous
; Exploration wells
; Late cretaceous
; Marine environment
; Middle Jurassic
; Southern North Sea
; Deposition
; Floods
; Seismic response
; Seismic waves
; Three dimensional
; Tectonics
; chronostratigraphy
; Cretaceous
; data set
; fault
; Jurassic
; movement
; Permian
; reconstruction
; rifting
; seismic data
; tectonostratigraphy
; three-dimensional modeling
; Atlantic Ocean
; Central Graben
; North Sea
Scopus学科分类: Energy
; Earth and Planetary Sciences
英文摘要: A three-dimensional seismic data set and published data from exploration wells were used to reconstruct the tectonostratigraphic evolution of the Mandal High area, southern North Sea, Norway. The Mandal High is an elongated southeastnorthwest-trending horst. Three fault families in the Lower Permian sequence, inherited from the basement structural grain of Caledonian origin, are interpreted: (1) a north-northwest-south-southeast-striking fault family, (2) a northeastsouthwest-striking fault family, and (3) a near east-west-striking fault family. In addition, an east-southeast-west-northweststriking fault family (4) that formed during Late Jurassic rifting and was reverse reactivated in the Late Cretaceous is interpreted. We suggest that inversion occurred because of small dextral motion along fault family 1. A final fault family (5) displays various strike orientations and is associated with salt movements. Seven chronostratigraphic sequences defined by well data and recognized on three-dimensional seismic data are interpreted and mapped: Early Permian rifting in a continental environment; Late Permian deposition of the Zechstein salt and flooding; Triassic continental rifting; uplift and erosion in the Middle Jurassic with deposition of shallow-marine and deltaic sediments; rifting and transgression in a deep-marine environment during the Late Jurassic; a post-rift phase in a marine environment during the Early Cretaceous; and flooding and deposition of the Chalk Group in the Late Cretaceous. An eighth sequence was interpreted-Paleogene-Neogene-but © 2013. The American Association of Petroleum Geologists. URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84879530494&doi=10.1306%2f12031212093&partnerID=40&md5=6449b78190f3b83b15d35447bbbd7e6d
Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/13246
Appears in Collections: 过去全球变化的重建 影响、适应和脆弱性 科学计划与规划 气候变化与战略 全球变化的国际研究计划 气候减缓与适应 气候变化事实与影响
There are no files associated with this item.
Recommended Citation:
Rossland A.,Escalona A.,Rolfsen R.. Permian-hobcene tectonostratigraphic evolution of the Mandal high, central graben, North Sea[J]. AAPG Bulletin,2013-01-01,97(6)