Petrology of the gabbro and sheeted basaltic intrusives at North Cape, New Zealand
The North Cape massif consists of a semi-conformable sequence of serpentinite, gabbro, sheeted sill and dike units, and pillow lavas. Although structurally disrupted, they can be interpreted in terms of an idealised ophiolite sequence and represent the most complete sequence in the Northland Ophioli...
Published in: | New Zealand Journal of Geology and Geophysics |
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Language: | English |
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Informa UK Limited
1996
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Online Access: | https://espace.library.uq.edu.au/view/UQ:703719 |
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ftunivqespace:oai:espace.library.uq.edu.au:UQ:703719 2023-05-15T17:37:56+02:00 Petrology of the gabbro and sheeted basaltic intrusives at North Cape, New Zealand Hopper, Derek J. Smith, Ian E. M. 1996-01-01 https://espace.library.uq.edu.au/view/UQ:703719 eng eng Informa UK Limited doi:10.1080/00288306.1996.9514721 issn:1175-8791 issn:0028-8306 Gabbro North Cape Northland Ophiolite Petrology Sheeted dikes Sheeted intrusives Tangihua Volcanics 1901 Earth and Planetary Sciences (miscellaneous) 1907 Geology 1908 Geophysics Journal Article 1996 ftunivqespace https://doi.org/10.1080/00288306.1996.9514721 2020-08-18T03:44:30Z The North Cape massif consists of a semi-conformable sequence of serpentinite, gabbro, sheeted sill and dike units, and pillow lavas. Although structurally disrupted, they can be interpreted in terms of an idealised ophiolite sequence and represent the most complete sequence in the Northland Ophiolite. Their age is considered to be Late Cretaceous - Paleocene on the basis of microfossils in associated sediments. Early Miocene K-Ar ages from igneous rocks are thought to reflect the time of emplacement as a thrust sheet of oceanic crust and upper mantle. The gabbros are divided into a lower unit characterised by well-developed cumulate layering and an upper unit which is massive; the sheeted sills and dikes are quartz-diorite and microgabbro interleaved with minor pillow lava. Two phases of alteration are observed, a pervasive low-grade greenschist metamorphism attributed to sea-water interaction after formation as oceanic crust, and an overprinting zeolitic alteration which is possibly post-emplacement. Their tholeiitic nature as well as overlapping geochemical compositions suggest that the gabbros and sheeted dikes and sills represent ditferent components of a single magmatic system related by simple fractionation processes. Several lines of evidence suggest that the magmas that formed the North Cape gabbro and sheeted intrusives have subduction-related chemical characteristics. In the gabbro, calcic plagioclase (An) and depleted Zr and Y abundances, and in the sheeted intrusives depleted high field strength element abundances relative to typical MORB, is indicative of a subduction signature. The presence of subduction-'elated characteristics within the Northland Ophiolite suggests that it may have originated at a back-arc basin rather than a major ocean ridge spreading centre. Article in Journal/Newspaper North Cape The University of Queensland: UQ eSpace New Zealand North Cape ENVELOPE(165.700,165.700,-70.650,-70.650) New Zealand Journal of Geology and Geophysics 39 3 389 402 |
institution |
Open Polar |
collection |
The University of Queensland: UQ eSpace |
op_collection_id |
ftunivqespace |
language |
English |
topic |
Gabbro North Cape Northland Ophiolite Petrology Sheeted dikes Sheeted intrusives Tangihua Volcanics 1901 Earth and Planetary Sciences (miscellaneous) 1907 Geology 1908 Geophysics |
spellingShingle |
Gabbro North Cape Northland Ophiolite Petrology Sheeted dikes Sheeted intrusives Tangihua Volcanics 1901 Earth and Planetary Sciences (miscellaneous) 1907 Geology 1908 Geophysics Hopper, Derek J. Smith, Ian E. M. Petrology of the gabbro and sheeted basaltic intrusives at North Cape, New Zealand |
topic_facet |
Gabbro North Cape Northland Ophiolite Petrology Sheeted dikes Sheeted intrusives Tangihua Volcanics 1901 Earth and Planetary Sciences (miscellaneous) 1907 Geology 1908 Geophysics |
description |
The North Cape massif consists of a semi-conformable sequence of serpentinite, gabbro, sheeted sill and dike units, and pillow lavas. Although structurally disrupted, they can be interpreted in terms of an idealised ophiolite sequence and represent the most complete sequence in the Northland Ophiolite. Their age is considered to be Late Cretaceous - Paleocene on the basis of microfossils in associated sediments. Early Miocene K-Ar ages from igneous rocks are thought to reflect the time of emplacement as a thrust sheet of oceanic crust and upper mantle. The gabbros are divided into a lower unit characterised by well-developed cumulate layering and an upper unit which is massive; the sheeted sills and dikes are quartz-diorite and microgabbro interleaved with minor pillow lava. Two phases of alteration are observed, a pervasive low-grade greenschist metamorphism attributed to sea-water interaction after formation as oceanic crust, and an overprinting zeolitic alteration which is possibly post-emplacement. Their tholeiitic nature as well as overlapping geochemical compositions suggest that the gabbros and sheeted dikes and sills represent ditferent components of a single magmatic system related by simple fractionation processes. Several lines of evidence suggest that the magmas that formed the North Cape gabbro and sheeted intrusives have subduction-related chemical characteristics. In the gabbro, calcic plagioclase (An) and depleted Zr and Y abundances, and in the sheeted intrusives depleted high field strength element abundances relative to typical MORB, is indicative of a subduction signature. The presence of subduction-'elated characteristics within the Northland Ophiolite suggests that it may have originated at a back-arc basin rather than a major ocean ridge spreading centre. |
format |
Article in Journal/Newspaper |
author |
Hopper, Derek J. Smith, Ian E. M. |
author_facet |
Hopper, Derek J. Smith, Ian E. M. |
author_sort |
Hopper, Derek J. |
title |
Petrology of the gabbro and sheeted basaltic intrusives at North Cape, New Zealand |
title_short |
Petrology of the gabbro and sheeted basaltic intrusives at North Cape, New Zealand |
title_full |
Petrology of the gabbro and sheeted basaltic intrusives at North Cape, New Zealand |
title_fullStr |
Petrology of the gabbro and sheeted basaltic intrusives at North Cape, New Zealand |
title_full_unstemmed |
Petrology of the gabbro and sheeted basaltic intrusives at North Cape, New Zealand |
title_sort |
petrology of the gabbro and sheeted basaltic intrusives at north cape, new zealand |
publisher |
Informa UK Limited |
publishDate |
1996 |
url |
https://espace.library.uq.edu.au/view/UQ:703719 |
long_lat |
ENVELOPE(165.700,165.700,-70.650,-70.650) |
geographic |
New Zealand North Cape |
geographic_facet |
New Zealand North Cape |
genre |
North Cape |
genre_facet |
North Cape |
op_relation |
doi:10.1080/00288306.1996.9514721 issn:1175-8791 issn:0028-8306 |
op_doi |
https://doi.org/10.1080/00288306.1996.9514721 |
container_title |
New Zealand Journal of Geology and Geophysics |
container_volume |
39 |
container_issue |
3 |
container_start_page |
389 |
op_container_end_page |
402 |
_version_ |
1766138150795608064 |