Neogene Tectonic Evolution of the Southwestern Alboran Basin as Inferred from Seismic Data Off Morocco
Neogene Tectonic Evolution of the Southwestern Alboran Basin as Inferred from Seismic Data Off Morocco
复制标题
摩洛哥近海地震数据推断的西南阿尔沃兰盆地新近纪构造演化
DOI:
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发表时间:
1997
期刊:
影响因子:
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通讯作者:
A. Bally
中科院分区:
文献类型:
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作者:
A. Chalouan;R. Saji;A. Michard;A. Bally
The southwestern part of the western Mediterranean Alboran Basin, including part of the Alboran ridge (Xaouen Bank), was investigated through the analysis of 28 intersecting multichannel seismic lines. The seismic stratigraphy is tied to the Amoco well El-Jebha 1. Five seismic units or subunits are described from the Quaternary to the middle (and lower?) Miocene. The acoustic basement is interpreted to be mainly Paleozoic and Triassic metamorphic rocks of the Alboran Domain nappes, and, in places, middle Miocene-Messinian calc-alkalic volcanics. In the depocenters, the thickness of the sedimentary infill (mostly clays and turbidites) exceeds 9 km. Normal faults of middle Miocene-Tortonian age are broadly parallel to the coast, and dip either seaward or landward. They were mostly inverted during pre- and post-Messinian episodes of compression, which formed a set of en echelon, north-verging faulted folds in the Alboran ridge area, in relation with sinistral movement along the offshore projection of the Jebha fault. After Pliocene subsidence, a final episode of compression reactivated the earlier folds and pushed the Alboran ridge onto the Moroccan slope. The complex structural history suggests many structural and stratigraphic potential hydrocarbon traps. A high-resolution seismic survey could lead to the definition of new exploration plays.