Warkworth Subgroup

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Geographic outcrop distribution of the previously recognised paleogeographi...

in USING MULTI-FORAMINIFERAL-PROXIES TO RESOLVE THE PALEOGEOGRAPHIC HISTORY OF A LOWER MIOCENE, SUBDUCTION-RELATED, SEDIMENTARY BASIN (WAITEMATA BASIN, NEW ZEALAND) > Journal of Foraminiferal Research

Published: 01 July 2016

; Edbrooke & Brook, 2009 ). The central part of the Waitemata Basin (Warkworth Subgroup) is divided into the following facies: basal transgressive facies (Kawau Subgroup); volcanic-poor flysch (East Coast Bays Formation); volcanic-rich flysch (Pakiri Formation); mixed volcanic-rich and volcanic-poor

Journal Article

USING MULTI-FORAMINIFERAL-PROXIES TO RESOLVE THE PALEOGEOGRAPHIC HISTORY OF A LOWER MIOCENE, SUBDUCTION-RELATED, SEDIMENTARY BASIN (WAITEMATA BASIN, NEW ZEALAND)

Bruce W. Hayward, Christopher M. Triggs

Journal: Journal of Foraminiferal Research

Publisher: Cushman Foundation for Foraminiferal Research

Published: 01 July 2016

Journal of Foraminiferal Research (2016) 46 (3): 285–313.

DOI: https://doi.org/10.2113/gsjfr.46.3.285

... ; Edbrooke & Brook, 2009 ). The central part of the Waitemata Basin (Warkworth Subgroup) is divided into the following facies: basal transgressive facies (Kawau Subgroup); volcanic-poor flysch (East Coast Bays Formation); volcanic-rich flysch (Pakiri Formation); mixed volcanic-rich and volcanic-poor...

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