Background, Objectives, and Principal Results of Drilling the Clastic Apron of Gran Canaria (VICAP)

Schmincke, H.-U.; Weaver, P. P. E.; Firth, J.V.; Baraza, J.; Bristow, J. F.; Brunner, Charlotte A; Carey, Steve; Coakley, Bernard; Fuller, Myron L.; Funck, Thomas; Gérard, Martine; Goldstrand, Patrick M.; Herr, B.; Hood, J. A. A.; Howe, Robert C.; Jarvis, Ian; Lebreiro, Susana Martin; Lindblom, Sten; Lykke‐Andersen, Holger; Maniscalco, Rosanna; Rothwell, Gar W.; Sblendorio-Levy, J.; Schneider, Jean Luc; Sumita, Mari; Taniguchi, Haruhito; Tu, P.; Wallace, Peigi

doi:10.2973/odp.proc.ir.157.102.1995

Proceedings of the Ocean Drilling Program 1995

DOI: 10.2973/odp.proc.ir.157.102.1995

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Background, Objectives, and Principal Results of Drilling the Clastic Apron of Gran Canaria (VICAP)

H.-U. Schmincke¹,

P. P. E. Weaver²,

J.V. Firth³

et al.

Abstract: BACKGROUND Volcanic aprons A volcanic apron peripheral to an oceanic island consists of three main facies above the central or core facies and is made up of extrusive and intrusive igneous rocks (Schmincke, 1994; Fig. 1):

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Background, Objectives, and Principal Results of Drilling the Clastic Apron of Gran Canaria (VICAP)

Abstract: BACKGROUND Volcanic aprons A volcanic apron peripheral to an oceanic island consists of three main facies above the central or core facies and is made up of extrusive and intrusive igneous rocks (Schmincke, 1994; Fig. 1):

Cited by 1 publication

References 21 publications

First seamount age evidence for significantly slower African plate motion since 19 to 30 Ma

First seamount age evidence for significantly slower African plate motion since 19 to 30 Ma

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