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Ngatamariki Field

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Journal Article
Journal: Interpretation
Published: 15 July 2016
Interpretation (2016) 4 (3): SJ87–SJ101.
...Francesco Civilini; Aasha Pancha; Martha Kane Savage; Steven Sewell; John Townend Abstract We have determined subsurface structure using the refraction microtremor (ReMi) method at the Ngatamariki geothermal field, Central North Island, New Zealand. The local geology is such that refraction...
FIGURES | View All (10)
Journal Article
Published: 01 August 1989
American Mineralogist (1989) 74 (7-8): 759–763.
...Patrick R. L. Browne; Sue F. Courtney; C. Peter Wood Abstract Chips ejected during the initial openings of Ngatamariki well, NM2, in the Taupo Volcanic Zone, New Zealand, consist of euhedral crystals of wairakite, prehnite, and Fe-rich epidote, plus rare quartz and pyrite. The shapes of some...
Image
Geologic map of the <span class="search-highlight">Ngatamariki</span> geothermal <span class="search-highlight">field</span>, showing surface lithologi...
Published: 01 March 2017
Fig. 2. Geologic map of the Ngatamariki geothermal field, showing surface lithologies and the locations of deep wells, hot springs, fault traces, field resistivity boundary, and cross section trace of Figure 3 . Coordinates in NZ Map Grid NZMG. The surface geological units are from Leonard et
Image
Geologic cross section of the <span class="search-highlight">Ngatamariki</span> geothermal <span class="search-highlight">field</span> showing A) the s...
Published: 01 March 2017
Fig. 3. Geologic cross section of the Ngatamariki geothermal field showing A) the stratigraphic lithological units and B) the hydrothermal alteration mineralogy. The top of the Tahorakuri Formation represents the paleosurface at the time of the Whakamaru ignimbrite deposition. Wells
Image
Geologic cross section of the <span class="search-highlight">Ngatamariki</span> geothermal <span class="search-highlight">field</span> showing A) the s...
Published: 01 March 2017
Fig. 3. Geologic cross section of the Ngatamariki geothermal field showing A) the stratigraphic lithological units and B) the hydrothermal alteration mineralogy. The top of the Tahorakuri Formation represents the paleosurface at the time of the Whakamaru ignimbrite deposition. Wells
Image
(a) The <span class="search-highlight">Ngatamariki</span> geothermal <span class="search-highlight">field</span>, located approximately 20 km northeast...
Published: 15 July 2016
Figure 1. (a) The Ngatamariki geothermal field, located approximately 20 km northeast of Taupo in the North Island of New Zealand. Panel b displays a map showing the locations of the deployed ReMi arrays (yellow lines) compared to nearby wells and the original structural cross section presented
Journal Article
Published: 26 November 2003
Canadian Journal of Earth Sciences (2003) 40 (11): 1643–1667.
...B.W. Mountain; L.G. Benning; J.A. Boerema Abstract To study the rate of growth of sinters in New Zealand hot springs, field experiments were conducted in seven geothermal areas. At Wairakei, fan-shaped subaqueous deposits of amorphous silica grow rapidly (350 kg a –1 m –2 of drain wall...
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Journal Article
Journal: Economic Geology
Published: 01 March 2017
Economic Geology (2017) 112 (2): 319–346.
...Fig. 2. Geologic map of the Ngatamariki geothermal field, showing surface lithologies and the locations of deep wells, hot springs, fault traces, field resistivity boundary, and cross section trace of Figure 3 . Coordinates in NZ Map Grid NZMG. The surface geological units are from Leonard et...
FIGURES | View All (13)
Image
Schematic time sequence depicting the volcanic and intrusive history for th...
Published: 01 March 2017
Fig. 4. Schematic time sequence depicting the volcanic and intrusive history for the host rocks of the Ngatamariki geothermal field based on U-Pb zircon ages (from Chambefort et al., 2014) . All ages have 2 s.d. uncertainties plotted. Symbols represent the top of the units. Lines connect the top
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Cross sections of the modern distribution of Paeroa Subgroup ignimbrites (s...
Published: 01 September 2014
Figure 8. Cross sections of the modern distribution of Paeroa Subgroup ignimbrites (see Fig. 7A ): (A) northwest-southeast, through the Te Weta and southern Paeroa fault blocks at the Te Kopia geothermal field, (B) from the Orakei Korako to Ngatamariki geothermal fields, and (C) west-east
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<span class="search-highlight">Field</span> photographs showing tree branches in spring pools. (A, B) Examples of...
Published: 27 November 2003
Fig. 13. Field photographs showing tree branches in spring pools. (A, B) Examples of tree branches in Iodine Pool, Waimangu (water temperature T = 88 °C, pH 8.9) and Hoani, Tokaanu ( T = 62.6 °C, pH 7.0), coated with opal-A precipitates. Wood inside branches has not been replaced. Branches up
Journal Article
Journal: Economic Geology
Published: 01 May 2016
Economic Geology (2016) 111 (3): 589–618.
... collected into the plastic bottle. Table 3 Trace Metal Analyses of Chloride Water Samples from Geothermal Wells Field Broadlands-Ohaaki Kawerau Mokai Ngatamariki Well Br47 Br47 Br47 Ka25 Ka25 Mk6 Mk6 Mk6 Mk6 Mk6 Nm4 Nm4 Nm4 Nm4 Date 10/1/2002 10/1/2002...
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A. Geothermal sample clumped isotope results compared to temperature constr...
Published: 01 December 2018
Fig. 2. A. Geothermal sample clumped isotope results compared to temperature constraints from T h and well fluid discharge measurements. Samples are sourced from three geothermal fields: Wairakei (WK-80), Broadlands-Ohaaki (BR-6, 13, 15, 21, 27, 42), and Ngatamariki (breccia). Discharge
Journal Article
Journal: GSA Bulletin
Published: 01 September 2014
GSA Bulletin (2014) 126 (9-10): 1131–1144.
...Figure 8. Cross sections of the modern distribution of Paeroa Subgroup ignimbrites (see Fig. 7A ): (A) northwest-southeast, through the Te Weta and southern Paeroa fault blocks at the Te Kopia geothermal field, (B) from the Orakei Korako to Ngatamariki geothermal fields, and (C) west-east...
FIGURES | View All (10)
Journal Article
Journal: SEG Discovery
Published: 01 January 2008
SEG Discovery (2008) (72): 1–12.
... their predominantly meteoric origin ( Giggenbach, 1995 ). The compositions from shallow wells at Ladolam, Lihir Island, Papua New Guinea, occupy the field labelled “Ladolam trend,” representing a mixing trend between local meteoric water and deep magmatic water ( Carman, 2003 ); the star represents the isotopic...
FIGURES | View All (5)
Journal Article
Journal: Economic Geology
Published: 01 December 2018
Economic Geology (2018) 113 (8): 1671–1678.
...Fig. 2. A. Geothermal sample clumped isotope results compared to temperature constraints from T h and well fluid discharge measurements. Samples are sourced from three geothermal fields: Wairakei (WK-80), Broadlands-Ohaaki (BR-6, 13, 15, 21, 27, 42), and Ngatamariki (breccia). Discharge...
FIGURES | View All (5)
Journal Article
Journal: Interpretation
Published: 15 July 2016
Interpretation (2016) 4 (3): SJi.
... understanding and enhancing geothermal systems without the cost of traditional seismic acquisition. Civilini et al. present a pilot study of the refraction microtremor method at the Ngatamariki geothermal field (central North Island, New Zealand), where refraction and reflection studies are hindered...
Journal Article
Journal: Geosphere
Published: 01 February 2014
Geosphere (2014) 10 (1): 185–206.
...–4C ) ( Leonard et al., 2010 ). Silicic plutonic bodies have been proposed as being widely present ( Evison et al., 1976 ; Stern, 1985 ); however, the only in-situ plutonic bodies identified are in the Ngatamariki geothermal field at 2.6 km or greater depth ( Fig. 4B ) ( Browne et al., 1992...
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Journal Article
Published: 27 November 2003
Canadian Journal of Earth Sciences (2003) 40 (11): 1549–1569.
...Fig. 13. Field photographs showing tree branches in spring pools. (A, B) Examples of tree branches in Iodine Pool, Waimangu (water temperature T = 88 °C, pH 8.9) and Hoani, Tokaanu ( T = 62.6 °C, pH 7.0), coated with opal-A precipitates. Wood inside branches has not been replaced. Branches up...
FIGURES | View All (14)
Journal Article
Journal: Geology
Published: 01 January 2017
Geology (2017) 45 (1): 43–46.
... samples investigated. In the vein host rock, the dominant matrix and void spaces were intensely silicified by secondary quartz and primary feldspar was replaced by patchy adularia pseudomorphs (Fig. DR2D). Geothermal fields are geographically stable features that exhibit thermal variability...
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