Contact for the resource

GNS Science

8039 record(s)
 
Type of resources
Available actions
Topics
Keywords
Contact for the resource
Provided by
Years
Formats
Representation types
Update frequencies
status
Scale
Resolution
From 1 - 10 / 8039
  • This dataset contains geospatial datasets for sedimentary basins in the Northwest Province (Taranaki, Deepwater Taranaki, and Reinga-Northland basins), produced and compiled as part of GNS Science's "Atlas of Petroleum Prospectivity" programme (APP). APP is synthesising the wealth of new and existing information and knowledge within GNS Science and other open-file sources, to produce a nationally-significant baseline reference dataset that summarises the current understanding of the petroleum prospectivity of New Zealand's offshore sedimentary basins. Polygon, point, and polyline features are organised thematically into Feature Datasets, each of which contains multiple Feature Classes. Raster datasets are included at the highest hierarchical level of the database. The co-ordinate system used for the database is New Zealand Transverse Mercator, based on the NZGD2000 datum. Database compilation was undertaken using ArcGIS 10.3.1 for Desktop (version 10.3.1.4959). For further information on these data, please refer to: Arnot, M.J. and Bland, K.J. et al. (Compilers), 2016. Atlas of Petroleum Prospectivity, Northwest Province: ArcGIS geodatabase and technical report. GNS Science Data Series 23b.

  • Aerial photography of the wider Kaikōura region captured in the flying season of 2016-2017. Coverage encompasses North Canterbury and Marlborough regions. This Imagery was commissioned by LINZ on behalf of GNS science, Environment Canterbury Regional Council, Marlborough District Council, Kaikoura District Council and Hurunui District Council for earthquake recovery purposes. It was captured by Aerial Surveys Ltd, Unit A1, 8 Saturn Place, Albany,0632, New Zealand. The dataset comprises:4-band (RGBI) orthomosaic supplied at 30cm pixel resolution (0.30m GSD) and can be obtained from LINZ (https://data.linz.govt.nz/layer/95549-kaikoura-030m-rural-aerial-photos-2016-2017/) The above is supplied in terms of New Zealand Transverse Mercator (NZTM) 2000 map projection. Cite data as: GNS Science, Environment Canterbury Regional Council, Marlborough District Council, Kaikōura District Council, Hurunui District Council, Waka Kotahi NZ Transport Agency, Earthquake Commission, Toitū Te Whenua Land Information New Zealand (LINZ) (2022). 2016-2017 Kaikoura 0.30m Rural Aerial Photos [Data set]. Collected by Aerial Surveys, distributed by LINZ. https://doi.org/10.21420/ZSJ5-N017

  • Supplementary Data Table 1 Otago and Marlborough schist, detrital zircon ages of schist protoliths U-Th-Pb isotopic ratios, measured and common-Pb corrected detrital zircon ages A) Western Otago: Samples 1-18 B) Marlborough: Samples 19-30 Supplementary Data Table 2 U-Pb zircon age data, southern New England Orogen granite suites: Samples 1-6 Key Points • Original protoliths are recognisable within the Haast Schist of New Zealand on the basis of distinctive detrital zircon age patterns. • The Aspiring Lithological Association (Otago Schist) of western Otago, is correlated with a similar belt of schistose rocks (Marlborough Schist) in western Marlborough, and both are assigned to a Waipapa Composite Terrane protolith of Jurassic to Late Triassic age. • The Jurassic-Late Triassic sandstones within Waipapa Composite Terrane are dominantly of granitoid provenance in eastern Australia. • Detrital zircons of Carboniferous age in Waipapa Composite Terrane support a possible New England Orogen provenance in northeastern NSW and southeastern Queensland, and also indicate possible primary sources for the gold and tungsten in the western Otago Schist and western Marlborough Schist. • This result is in marked contrast to eastern Otago Schist where the protolith is Rakaia Terrane of Late Triassic age and whose provenance is in central-eastern Queensland.

  • LiDAR was commissioned by Toitū Te Whenua Land Information New Zealand on behalf of GNS Science, Environment Canterbury Regional Council, Marlborough District Council, Kaikoura District Council, Hurunui District Council, Waka Kotahi NZ Transport Agency, and the Earthquake Commission for earthquake recovery purposes for Kaikōura. LiDAR was captured by AAM Ltd after the 14 November 2016 earthquake. The dataset was generated by AAM and their subcontractors. Data management and distribution is by Toitū Te Whenua Land Information New Zealand Survey Date: 03/12/2016 - 06/01/2017 Point Cloud Data are available through OpenTopography (https://portal.opentopography.org/datasetMetadata?otCollectionID=OT.102022.2193.1) Prepared DEM files are available through the LINZ Data Service (https://data.linz.govt.nz/layer/110632-canterbury-kaikoura-lidar-1m-dem-2016/) Coordinate System: Horizontal: NZTM2000 NZGD2000 version 20160701 Vertical: NZVD2016 Imagery is supplied in terms of NZTM NZGD2000 version 20160701. The ground sample distance of the orthophotos is 20cm. Cite data as: GNS Science, Environment Canterbury Regional Council, Marlborough District Council, Kaikōura District Council, Hurunui District Council, Waka Kotahi NZ Transport Agency, Earthquake Commission, Toitū Te Whenua Land Information New Zealand (LINZ) (2022). Kaikōura, Canterbury, New Zealand 2016. Collected by AAM, distributed by OpenTopography and LINZ. https://doi.org/10.5069/G9HD7SWJ

  • Orthophotography for the Canterbury region taken in the flying season (summer period) 2014 - 2015. Coverage encompassed the Hurunui, and Kaikoura council areas. Imagery was captured for the ‘Environment Canterbury’ by Aerial Surveys Ltd, Unit A1, 8 Saturn Place, Albany,0632, New Zealand. The dataset comprises:4-band (RGBI) orthomosaic supplied at 30cm pixel resolution (0.30m GSD) and can be obtained from LINZ (https://data.linz.govt.nz/layer/52602-canterbury-03m-rural-aerial-photos-2014-2015/) The above is supplied in terms of New Zealand Transverse Mercator (NZTM) 2000 map projection. Cite data as: Environment Canterbury (2015). Canterbury 0.3m Rural Aerial Photos (2014-2015) [Data set]. Collected by Aerial Surveys, distributed by LINZ. https://doi.org/10.21420/K3H6-Z038

  • This vector data layer spatially represents chronostratigraphic grid based on the International Chronostratigraphic Chart (v 2021/10). Updates to this information areavailable at www.stratigraphy.org. This gridwas constructed using EPSG:4978 (WGS 84). It is also suitable for projection in EPSG:3031 (WGS 84/Antarctic Polar Stereographic). DOI https://doi.org/10.21420/7SH7-6K05

  • Downstream infrastructure Maui offshore platforms; Tui and Maari FPSOs; Pohokura, Maari and Kupe unmanned platforms. Eight onshore production stations in Taranaki. North Island gas pipeline network, including pipelines to Gisborne and Hastings. Oil refinery and port at Marsden Point, Whangarei, with connections to the North Island gas pipeline network and a liquids pipeline to Auckland.

  • This collection of datasets contains the 1:50 000 geological data for the Middlemarch area, East Otago, New Zealand (Topo50 sheet CD16). They spatially represents an interpretation of geological and geophysical information compiled from new field work and existing data. The mapping frame for the majority of datasets is defined as surface geology (i.e. the bedrock and superficial deposits that would be visible if the overlying soil was removed or are exposed at the topographic surface). The data structure complies with the GeoSciML Portrayal standard where one exists and fields required by that standard were populated using the CGI Controlled Vocabulary (2012-11). The data should not be used at scales beyond that for which it was prepared. The spatial accuracy is estimated to be no better than +/- 100 m. The datasets were produced by GNS Science and are associated with Martin, A.P.; Cox, S.C.; Smith Lyttle, B. 2016: Geology of the Middlemarch area 1:50 000. GNS Science geological map 5. Lower Hutt, New Zealand. GNS Science.

  • This file comprises a NZ wide velocity derived from InSAR and GNSS data between 2003 and 2011 published in “ Hamling, I, J., Wright, T. J., Hreinsdottir, S., Wallace, L. M., 2021 A snapshot of New Zealand's dynamic deformation field from Envisat InSAR and GNSS observations between 2003 and 2011 Geophysical Research Letters. The file contains the full InSAR velocities, standalon GNSS over the same period and coastal Vertical Land Movement as detailed in the manuscrtipt DOI: https://doi.org/10.21420/E1C1-MQ19 Cite data as: GNS Science. (2021). A snapshot of New Zealand's dynamic deformation field from Envisat InSAR and GNSS observations between 2003 and 2011 [Data set]. GNS Science. https://doi.org/10.21420/E1C1-MQ19

  • This Feature Class contains polygon features that summarise the exploration potential of the Miocene succession within sedimentary basins in the Northwest Province (Taranaki, Deepwater Taranaki, and Reinga-Northland basins). Areas where all of the requirements for oil or gas accumulation are present are indicated as having high exploration potential. Areas where all the requirements are not optimum, but may be present are indicated as areas of moderate exploration potential. Areas of low exploration potential indicates that on the basis of currently available open-file information there is a high risk for one or more of the petroleum systems elements not being able to effectively contribute to the petroleum system in that area. It is important to note that a rating of low exploration potential does not conclusively rule it out; rather, there is a high degree of uncertainty associated with presence of one or more of the petroleum system elements. For any given prospective area, more detailed work and data acquisition would be required. For more information about these data please refer to: Arnot, M.J. and Bland, K.J. et al. (Compilers), 2016. Atlas of Petroleum Prospectivity, Northwest Province: ArcGIS geodatabase and technical report. GNS Science Data Series 23b.