ALBORAN SEA LATE CENOZOIC TECTONIC AND STRATIGRAPHIC EVOLUTION

被引：72
|
作者：
MALDONADO, A
CAMPILLO, AC
MAUFFRET, A
ALONSO, B
WOODSIDE, J
CAMPOS, J
机构：
[1] UNIV PARIS 06,DEPT GEODYNAM TECTON & ENVIRONMENT,CNRS,F-75252 PARIS 05,FRANCE
[2] UNIV GRANADA,CSIC,INST ANDALUZ GEOL MEDITERRANEA,DEPT GEODINAM,GRANADA,SPAIN
[3] FREE UNIV AMSTERDAM,1081 HV AMSTERDAM,NETHERLANDS
来源：
GEO-MARINE LETTERS | 1992年 / 12卷 / 2-3期
关键词：
D O I：
10.1007/BF02084930
中图分类号：
P [天文学、地球科学];
学科分类号：
07 ;
摘要：
Analysis of airgun seismic profiles from the Alboran Sea reveals a complex morphostructure with margins, basins, and structural highs. North of the Alboran Ridge, south-facing margins have a passive style of evolution, with thick progradational sequences of post-Messinian deposits, whereas north-facing margins are tectonized along structural highs with reduced sediment cover. Basins are extensional features developed since the Early Miocene by mechanisms of tectonic escape and pull-apart, under generalized northwest-southeast to north-south compression. Depositional sequences in this semi-land-locked sea were controlled by the local tectonism and influenced by global sea-level oscillations.
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页码：179 / 186
页数：8
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