DOI: 10.1306/03091211087
Scopus记录号: 2-s2.0-84869485100
论文题名: Tectonostratigraphic evolution of the Jurassic extensional basins of the eastern southern Alps and Adriatic foreland based on an integrated study of surface and subsurface data
作者: Masetti D. ; Fantoni R. ; Romano R. ; Sartorio D. ; Trevisani E.
刊名: AAPG Bulletin
ISSN: 0149-1724
EISSN: 1558-9454
出版年: 2012
发表日期: 2012
卷: 96, 期: 11 起始页码: 2065
结束页码: 2089
语种: 英语
Scopus关键词: Adriatic
; Carbonate platforms
; Central Italy
; Early Jurassic
; Geophysical data
; Jurassic
; Northern Adriatic
; Northern Adriatic Sea
; Paleogeography
; Po plain
; Seismic profiles
; Subsurface data
; Synsedimentary
; Accidents
; Seismic waves
; Stratigraphy
; carbonate platform
; drilling
; extensional tectonics
; foreland basin
; Jurassic
; paleogeography
; subsurface flow
; synsedimentary tectonics
; tectonostratigraphy
; Adriatic Sea
; Alps
; Mediterranean Sea
Scopus学科分类: Energy
; Earth and Planetary Sciences
英文摘要: Successions that characterize the eastern southern Alps have been compared with coeval units drilled in the Alpine foreland (Po and Véneto plains, northern Adriatic Sea). The eastern southern Alps are composed of a carbonate platform-plateau, drowned in the Early Jurassic (Trento platform and plateau); a basin formed in the Early Jurassic (Belluno Basin) and a carbonate platform that lasted from the Jurassic to the Cretaceous (Friuli platform). Integration of stratigraphie and geophysical data illustrates the extensional architecture of the Alpine foreland subsurface. At the beginning of the Jurassic, peritidal successions were widespread everywhere except for the Belluno Basin. A reorganization of the Early Jurassic paleogeography affected the southern Alps around the Sinemurian-Pliensbachian boundary: the Pliensbachian successions were deposited in the central-western areas of the Trento platform whereas, elsewhere in the same platform and in the northern Friuli platform, Pliensbachian units are missing, replaced by an unconformity surface covered by crinoidal sands that have also been found in the subsurface. The Belluno Basin is recognizable in seismic profiles under the Véneto Plain. Southward (northern Adriatic Sea and Po plain), the basin between the Trento and the Friuli platforms, here called the "northern Adriatic Basin," possesses a stratigraphy different from that of the Belluno Basin. The northern Adriatic Basin drowned later, and seismic profiles indicate that it was wider and bounded by groups of small synsedimentary faults instead of the major faults displacing the Belluno Basin. The northern Adriatic Basin can be interpreted as the northeastern extension of the Umbro-Marchean Basin of central Italy. Copyright ©2012. The American Association of Petroleum Geologists. All rights reserved. URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84869485100&doi=10.1306%2f03091211087&partnerID=40&md5=8395d546d78836fdd8b0493378d59cb2
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/13294
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
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Recommended Citation:
Masetti D.,Fantoni R.,Romano R.,et al. Tectonostratigraphic evolution of the Jurassic extensional basins of the eastern southern Alps and Adriatic foreland based on an integrated study of surface and subsurface data[J]. AAPG Bulletin,2012-01-01,96(11)