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Kawau Subgroup

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Interpretation of the lower Miocene paleogeography of the greater Auckland ...

Interpretation of the lower Miocene paleogeography of the greater Auckland ...

Published: 01 July 2016
show inferred transport routes of displaced shallow-water faunas in coarse sediment deposits within the basin sequences. Present day coastline is shown in white. Some associations that only occur in the lower (Kawau Subgroup) parts of the basin fill are not represented.
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Geographic outcrop distribution of the previously recognised paleogeographi...

Geographic outcrop distribution of the previously recognised paleogeographi...

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
Published: 01 July 2016
Journal of Foraminiferal Research (2016) 46 (3): 285–313.
DOI: https://doi.org/10.2113/gsjfr.46.3.285
... show inferred transport routes of displaced shallow-water faunas in coarse sediment deposits within the basin sequences. Present day coastline is shown in white. Some associations that only occur in the lower (Kawau Subgroup) parts of the basin fill are not represented. ...
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“MONOSPECIFIC” AND NEAR-MONOSPECIFIC BENTHIC FORAMINIFERAL FAUNAS, NEW ZEALAND

Bruce W. Hayward
Published: 01 July 2014
Journal of Foraminiferal Research (2014) 44 (3): 300–315.
DOI: https://doi.org/10.2113/gsjfr.44.3.300
... (~300–800-μm test diameter) of extinct A. aucklandica occur quite commonly in early Miocene coarse sedimentary rocks around Auckland. Some of these appear to be near in situ in pebbly sandstone (R09/f58, S09/f4) close to the base of the transgressive Waitemata Group sequence (Kawau Subgroup...
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Engineering geomorphology of coastal landslides at Limestone Downs, North Island, New Zealand

Amanda Mueller, Lloyd Simmons, Martin S. Brook
Published: 30 October 2024
Quarterly Journal of Engineering Geology and Hydrogeology (2024) 57 (4): qjegh2024-046.
DOI: https://doi.org/10.1144/qjegh2024-046
... 2001 ). The Te Akatea Formation is overlain by early Miocene Waitemata Group rocks resting on a flat erosional surface. This basal Waitemata Group unit c . 2 km further north is a c . 8 m-thick shelly calcareous sandstone of the Kawau Subgroup ( Hayward and Brook 1984 ). However, at the Limestone...
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RECENT LITERATURE ON FORAMINIFERA

Jennifer A. Jett
Published: 01 July 2000
Journal of Foraminiferal Research (2000) 30 (3): 246–249.
DOI: https://doi.org/10.2113/0300246
... sequence, Matheson’s Bay, Leigh, Auckland.—Tane, v. 37, 1999, p. 43–67, 10 figures, 1 appendix.—“Sixty-three macrofossil taxa are recorded from early Miocene Kawau Subgroup (Waitemata Group) sequences at Mathesons Bay, Leigh. Fossils derived from intertidal, shallow subtidal, and inner shelf rocky reefs...
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Detrital zircon geochronology and sandstone provenance of basement Waipapa Terrane (Triassic–Cretaceous) and Cretaceous cover rocks (Northland Allochthon and Houhora Complex) in northern North Island, New Zealand

C. J. ADAMS, N. MORTIMER, H. J. CAMPBELL, W. L. GRIFFIN
Published: 16 July 2012
Geological Magazine (2013) 150 (1): 89–109.
DOI: https://doi.org/10.1017/S0016756812000258
... 4 7 e 250 ± 2 5 9 f 262 ± 3 4 7 55 (9B) KWI1 (R23365) KAWAU ISLAND, beach, west side, Grid Ref.: R09752319 a 162 ± 3 8 35 23 (9C) ADMX2 (R20840) SANDY BAY, Motutapu Island, Grid Ref.: R10/815939 a 226 ± 1 25 28 88 b...
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