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= Geologic map of the Paeroa Fault block and surrounding area, Taupo Volcanic Zone, New Zealand =
{"@context": "https://schema.org", "@type": "CreativeWork", "additionalType": "USGS Numbered Series", "name": "Geologic map of the Paeroa Fault block and surrounding area, Taupo Volcanic Zone, New Zealand", "identifier": [{"@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "ofr20201021", "url": "https://pubs.usgs.gov/publication/ofr20201021"}, {"@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70208812}, {"@type": "PropertyValue", "propertyID": "DOI", "value": "10.3133/ofr20201021", "url": "https://doi.org/10.3133/ofr20201021"}], "inLanguage": "en", "isPartOf": [{"@type": "CreativeWorkSeries", "name": "Open-File Report"}], "datePublished": "2020", "dateModified": "2020-03-20", "abstract": "The Taupo Volcanic Zone (TVZ), New Zealand, is the most productive area of explosive silicic volcanism in the world. Faulted early and middle Pleistocene volcanic products are generally concealed beneath voluminous, generally unfaulted, younger volcanic products. An exception is the southeast margin of the TVZ where the two parallel, northeast-trending Paeroa and Te Weta Fault blocks expose Quaternary volcanic products consisting predominantly of caldera-related, rhyolitic ignimbrites and lacustrine sediments. The Taupo-Reporoa Basin is situated along the eastern part of the map area, and its northernmost part underwent collapse to form Reporoa Caldera.The Paeroa Fault block is the largest exposed fault block within the TVZ, and it encompasses early and middle Pleistocene ignimbrites and sedimentary deposits that are buried throughout the Taupo-Reporoa Basin to the east. This map displays the volcanic and sedimentary geology of ~430 km2 of the Paeroa Fault block and the adjacent Te Weta Fault block at a scale of 1:50,000. Volcanic and sedimentary rocks are divided into the Reporoa Group, Whakamaru Group, and Huka Group (from oldest to youngest), which are overlain by relatively unfaulted late Pleistocene and Holocene surficial volcanic and sedimentary deposits.", "description": "1 Map: 50.22 x  34.79 inches; Data Release", "publisher": {"@type": "Organization", "name": "U.S. Geological Survey"}, "author": [{"@type": "Person", "name": "Downs, Drew T. ddowns@usgs.gov", "givenName": "Drew T.", "familyName": "Downs", "email": "ddowns@usgs.gov", "identifier": {"@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0002-9056-1404", "url": "https://orcid.org/0000-0002-9056-1404"}, "affiliation": [{"@type": "Organization", "name": "Volcano Science Center", "url": "https://www.usgs.gov/centers/volcano-science-center"}]}, {"@type": "Person", "name": "Leonard, Graham S.", "givenName": "Graham S.", "familyName": "Leonard", "affiliation": [{"@type": "Organization", "name": "GNS Science, New Zealand"}]}, {"@type": "Person", "name": "Wilson, Colin J. N.", "givenName": "Colin J. N.", "familyName": "Wilson", "affiliation": [{"@type": "Organization", "name": "Victoria University, PO Box 600, Wellington 6140, New Zealand"}]}, {"@type": "Person", "name": "Rowland, Julie V", "givenName": "Julie V", "familyName": "Rowland", "identifier": {"@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0002-6578-5035", "url": "https://orcid.org/0000-0002-6578-5035"}, "affiliation": [{"@type": "Organization", "name": "University of Auckland"}]}], "funder": [{"@type": "Organization", "name": "Volcano Science Center", "url": "https://www.usgs.gov/centers/volcano-science-center"}], "spatialCoverage": [{"@type": "Place", "additionalType": "country", "name": "New Zealand", "url": "https://geonames.org/2186224"}, {"@type": "Place", "geo": [{"@type": "GeoShape", "additionalProperty": {"@type": "PropertyValue", "name": "GeoJSON", "value": {"type": "FeatureCollection", "features": [{"type": "Feature", "properties": {}, "geometry": {"type": "Polygon", "coordinates": [[[165.948486328125, -46.72103466129568], [170.7550048828125, -46.72103466129568], [170.7550048828125, -44.15462243076732], [165.948486328125, -44.15462243076732], [165.948486328125, -46.72103466129568]]]}}]}}}, {"@type": "GeoCoordinates", "latitude": -45.437828546031504, "longitude": 168.35174560546875}]}]}
The Taupo Volcanic Zone (TVZ), New Zealand, is the most productive area of explosive silicic volcanism in the world. Faulted early and middle Pleistocene volcanic products are generally concealed beneath voluminous, generally unfaulted, younger volcanic products. An exception is the southeast margin of the TVZ where the two parallel, northeast-trending Paeroa and Te Weta Fault blocks expose Quaternary volcanic products consisting predominantly of caldera-related, rhyolitic ignimbrites and lacustrine sediments. The Taupo-Reporoa Basin is situated along the eastern part of the map area, and its northernmost part underwent collapse to form Reporoa Caldera.
 
The Paeroa Fault block is the largest exposed fault block within the TVZ, and it encompasses early and middle Pleistocene ignimbrites and sedimentary deposits that are buried throughout the Taupo-Reporoa Basin to the east. This map displays the volcanic and sedimentary geology of ~430 km<sup>2</sup> of the Paeroa Fault block and the adjacent Te Weta Fault block at a scale of 1:50,000. Volcanic and sedimentary rocks are divided into the Reporoa Group, Whakamaru Group, and Huka Group (from oldest to youngest), which are overlain by relatively unfaulted late Pleistocene and Holocene surficial volcanic and sedimentary deposits.

Revision as of 19:10, 15 July 2024

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