The Celtic Deep-Sea Fan: stratigraphy and sedimentary evolution

被引：22

作者：

Droz, L

Auffret, GA

Savoye, B

Bourillet, JF

机构：

[1] European Univ Inst, UMR 6538, F-29280 Plouzane, France

[2] IFREMER, DRO, GM, Lab Environm Sedimentaires, F-29280 Plouzane, France

来源：

COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II FASCICULE A-SCIENCES DE LA TERRE ET DES PLANETES | 1999年 / 328卷 / 03期

关键词：

deep-sea fan; Celtic margin; North Atlantic; seismic stratigraphy;

D O I：

10.1016/S1251-8050(99)80093-7

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

Seismic data collected on the Celtic Fan during Sedifan cruises (European Program Enam II), stratigraphically correlated to DSDP site 400 (leg 48) show that fan deposition was initialed during the Early Miocene. It progressively extended towards the middle of the Bay of Biscay during the Plio-Quaternary. The fan includes 3 main seismic units with several channel/levee bodies disturbed by mass-movement deposits. Depocenters shifted several times, and the present-day morphology ultimately results from a last shift of detritic inputs to the Whittard System. (C) Academie des sciences / Elsevier, Paris.

引用

页码：173 / 180

页数：8

共 11 条

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[2]

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[3]

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[4]

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[5]

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