Primary or secondary distal volcaniclastic turbidites: how to make the distinction? An example from the Miocene of New Zealand (Mahia Peninsula, North Island)-Reference-Cited by-同舟云学术

Primary or secondary distal volcaniclastic turbidites: how to make the distinction? An example from the Miocene of New Zealand (Mahia Peninsula, North Island)

Published:2001-12 Issue:1-2 Volume:145 Page:1-22
ISSN:0037-0738
Container-title:Sedimentary Geology
language:en
Short-container-title:Sedimentary Geology

Author:

Schneider Jean-Luc,Le Ruyet Anthony,Chanier Frank,Buret Christophe,Ferrière Jacky,Proust Jean-Noël,Rosseel Jean-Baptiste

Publisher

Elsevier BV

Subject

Stratigraphy,Geology

Reference68 articles.

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3. The New Zealand Neogene Forearc Basins;Ballance,1993

4. Sedimentology of Some Flysch Deposits: A Graphic Approach to Facies Interpretation;Bouma,1962

5. Depositional controls and characteristics of subaqueous bedded volcaniclastics of the Lower Devonian Snowy River Volcanics;Bull;Sedim. Geol.,1991

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