Robertson, Alastair H. F. (1998): Significance of lower Pliocene mass-flow deposits for the timing and process of collision of the Eratosthenes Seamount with the Cyprus active margin

Leg/Site/Hole:
ODP 160
Identifier:
2000-003476
georefid

10.2973/odp.proc.sr.160.038.1998
doi

Creator:
Robertson, Alastair H. F.
University of Edinburgh, Department of Geology and Geophysics, Edinburgh, United Kingdom
author

Identification:
Significance of lower Pliocene mass-flow deposits for the timing and process of collision of the Eratosthenes Seamount with the Cyprus active margin
1998
In: Robertson, Alastair H. F., Emeis, Kay-Christian, Richter, Carl, Blanc-Valleron, Marie-Madeleine, Bouloubassi, Ioanna, Brumsack, Hans-Juergen, Cramp, Adrian, de Lange, Gert Jan, Di Stefano, Enrico, Flecker, Rachel, Frankel, Edgar, Howell, Michael W., Janecek, Thomas R., Jurado-Rodriguez, Maria Jose, Kemp, Alan E. S., Koizumi, Itaru, Kopf, Achim, Major, Candace O., Mart, Yossi, Pribnow, Daniel F. C., Rabaute, Alain, Roberts, Andrew P., Rullkoetter, Juergen H., Sakamoto, Tatsuhiko, Spezzaferri, Silvia, Staerker, T. Scott, Stoner, Joseph S., Whiting, Brian M., Woodside, John M., Miller, Christine M. (editor), Riegel, Ruth N. (editor), Proceedings of the Ocean Drilling Program, scientific results; Mediterranean I; covering the cruises of the drilling vessel JOIDES Resolution, Las Palmas, Gran Canaria, to Naples, Italy, sites 963-973, 7 March-3 May 1995
Texas A & M University, Ocean Drilling Program, College Station, TX, United States
160
465-481
Coverage:Geographic coordinates:
North:38.0000
West:30.0000East: 34.0000
South:34.0000

Solid-earth geophysics; active margins; Asia; carbonate rocks; Cenozoic; Cyprus; depositional environment; diagenesis; East Mediterranean; Eratosthenes Seamount; Leg 160; lower Pliocene; marine sediments; Mediterranean Sea; Middle East; Neogene; Ocean Drilling Program; plate collision; plate tectonics; Pliocene; Polis Graben; sedimentary rocks; sedimentary structures; sediments; tectonics; Tertiary; Troodos Ophiolite;

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