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ADAMS, C. J., MORTIMER, N., CAMPBELL, H. J., GRIFFIN, W. L. (2013) 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. Geological Magazine, 150 (1) 89-109 doi:10.1017/s0016756812000258

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Reference TypeJournal (article/letter/editorial)
TitleDetrital 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
JournalGeological Magazine
AuthorsADAMS, C. J.Author
MORTIMER, N.Author
CAMPBELL, H. J.Author
GRIFFIN, W. L.Author
Year2013 (January)Volume150
Issue1
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756812000258Search in ResearchGate
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Mindat Ref. ID260708Long-form Identifiermindat:1:5:260708:9
GUID0
Full ReferenceADAMS, C. J., MORTIMER, N., CAMPBELL, H. J., GRIFFIN, W. L. (2013) 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. Geological Magazine, 150 (1) 89-109 doi:10.1017/s0016756812000258
Plain TextADAMS, C. J., MORTIMER, N., CAMPBELL, H. J., GRIFFIN, W. L. (2013) 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. Geological Magazine, 150 (1) 89-109 doi:10.1017/s0016756812000258
In(2013, January) Geological Magazine Vol. 150 (1) Cambridge University Press (CUP)
Abstract/NotesAbstractDetrital zircon U–Pb ages are reported for 14 sandstones of mainly Cretaceous age from the Northland Allochthon, Houhora Complex and Waipapa Terrane of northern North Island, New Zealand. Results from the Waipapa Terrane samples, selected from sequences in the Bay of Plenty, Coromandel Peninsula and Great Barrier Island, show that deposition continued into late Early Cretaceous time and, as in the Torlesse Composite Terrane, finally waned at c. 110–114 Ma. Upper Lower Cretaceous and Upper Cretaceous sedimentary successions in the Houhora Complex and Northland Allochthon have dominant sediment sources derived from local, contemporary volcanism, with a minor older contribution from the Murihiku Terrane to the west. As in eastern North Island, upper Upper Cretaceous sandstones lack major Albian magmatic components and their sources are solely in the Murihiku Terrane, and possibly the Western Province. We propose a Cretaceous palaeogeographic model that invokes a recently extinct orogen and a partially submerged continental borderland, dissected by rivers supplying submarine fans.


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To cite: Ralph, J., Von Bargen, D., Martynov, P., Zhang, J., Que, X., Prabhu, A., Morrison, S. M., Li, W., Chen, W., & Ma, X. (2025). Mindat.org: The open access mineralogy database to accelerate data-intensive geoscience research. American Mineralogist, 110(6), 833–844. doi:10.2138/am-2024-9486.
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