Relevant bibliographies by topics / Whakatane

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters

Academic literature on the topic 'Whakatane'

Author: Grafiati
Published: 4 June 2021
Last updated: 19 February 2022

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Journal articles on the topic "Whakatane"

1

Freudenthal, Emmanuel, Maurizio Farhan Ferrari, Justin Kenrick, and Adrian Mylne. "The Whakatane Mechanism: Promoting Justice in Protected Areas." Nomadic Peoples 16, no. 2 (December 31, 2012): 84–94. http://dx.doi.org/10.3167/np.2012.160207.

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2

Wright, I. C. "Late Quaternary faulting of the offshore Whakatane Graben, Taupo Volcanic Zone, New Zealand." New Zealand Journal of Geology and Geophysics 33, no. 2 (April 1990): 245–56. http://dx.doi.org/10.1080/00288306.1990.10425682.

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3

Holt, Katherine A., David J. Lowe, Alan G. Hogg, and R. Clel Wallace. "Distal occurrence of mid-Holocene Whakatane Tephra on the Chatham Islands, New Zealand, and potential for cryptotephra studies." Quaternary International 246, no. 1-2 (December 2011): 344–51. http://dx.doi.org/10.1016/j.quaint.2011.06.026.

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4

Lamarche, Geoffroy, Philip M. Barnes, and Jonathan M. Bull. "Faulting and extension rate over the last 20,000 years in the offshore Whakatane Graben, New Zealand continental shelf." Tectonics 25, no. 4 (July 12, 2006): n/a. http://dx.doi.org/10.1029/2005tc001886.

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5

Nixon, Casey W., Jonathan M. Bull, and David J. Sanderson. "Localized vs distributed deformation associated with the linkage history of an active normal fault, Whakatane Graben, New Zealand." Journal of Structural Geology 69 (December 2014): 266–80. http://dx.doi.org/10.1016/j.jsg.2014.06.005.

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6

Zhang, Jian, Dick Beetham, Grant Dellow, John X. Zhao, and Graeme H. McVerry. "Empirical models for predicting lateral spreading and evaluation using New Zealand data." Bulletin of the New Zealand Society for Earthquake Engineering 41, no. 1 (March 31, 2008): 10–23. http://dx.doi.org/10.5459/bnzsee.41.1.10-23.

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A New empirical model has been developed for predicting liquefaction-induced lateral spreading displacement and is a function of response spectral displacements and geotechnical parameters. Different from the earlier model of Zhang and Zhao (2005), the application of which was limited to Japan and California, the new model can potentially be applied anywhere if ground shaking can be estimated (by using local strong-motion attenuation relations). The new model is applied in New Zealand where the response spectral displacement is estimated using New Zealand strong-motion attenuation relations (McVerry et al. 2006). The accuracy of the new model is evaluated by comparing predicted lateral displacements with those which have been measured from aerial photos or the width of ground cracks at the Landing Road bridge, the James Street loop, the Whakatane Pony Club and the Edgecumbe road and rail bridges sites after the 1987 Edgecumbe earthquake. Results show that most predicted errors (defined as the ratio of the difference between the measured and predicted lateral displacements to the measured one) from the new model are less than 40%. When compared with earlier models (Youd et al. 2002, Zhang and Zhao 2005), the new model provides the lowest mean errors.
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7

Lowe, David J. "Revision of the age and stratigraphic relationships of Hinemaiaia Tephra and Whakatane Ash, North Island, New Zealand, using distal occurrences in organic deposits." New Zealand Journal of Geology and Geophysics 29, no. 1 (January 1986): 61–73. http://dx.doi.org/10.1080/00288306.1986.10427523.

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8

Kobayashi, Tetsuo, Ian Nairn, Vicki Smith, and Phil Shane. "Proximal stratigraphy and event sequence of the c. 5600 cal. yr BP Whakatane rhyolite eruption episode from Haroharo volcano, Okataina Volcanic Centre, New Zealand." New Zealand Journal of Geology and Geophysics 48, no. 3 (September 2005): 471–90. http://dx.doi.org/10.1080/00288306.2005.9515127.

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9

Orense, Rolando, Mohammad Asadi, Mark Stringer, and Michael Pender. "EVALUATING LIQUEFACTION POTENTIAL OF PUMICEOUS DEPOSITS THROUGH FIELD TESTING: CASE STUDY OF THE 1987 EDGECUMBE EARTHQUAKE." Bulletin of the New Zealand Society for Earthquake Engineering 53, no. 2 (June 1, 2020): 101–10. http://dx.doi.org/10.5459/bnzsee.53.2.101-110.

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Pumice materials, which are problematic from an engineering viewpoint, are widespread in the central part of the North Island. Considering the impacts of the 2010-2011 Christchurch earthquakes, a clear understanding of their properties under earthquake loading is necessary. For example, the 1987 Edgecumbe earthquake showed evidence of localised liquefaction of sands of volcanic origin. To elucidate on this, research was undertaken to investigate whether existing empirical field-based methods to evaluate the liquefaction potential of sands, which were originally developed for hard-grained soils, are applicable to crushable pumice-rich deposits. For this purpose, two sites, one in Whakatane and another in Edgecumbe, were selected where the occurrence of liquefaction was reported following the Edgecumbe earthquake. Manifestations of soil liquefaction, such as sand boils and ejected materials, have been reported at both sites. Field tests, including cone penetration tests (CPT), shear-wave velocity profiling, and screw driving sounding (SDS) tests were performed at the sites. Then, considering estimated peak ground accelerations (PGAs) at the sites based on recorded motions and possible range of ground water table locations, liquefaction analysis was conducted at the sites using available empirical approaches. To clarify the results of the analysis, undisturbed soil samples were obtained at both sites to investigate the laboratory-derived cyclic resistance ratios and to compare with the field-estimated values. Research results clearly showed that these pumice-rich soils do not fit existing liquefaction assessment frameworks and alternate methods are necessary to characterise them.
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10

Khan, Afrasyab, and Jagdish Prasad. "Colorectal cancer presentation in eastern Bay of Plenty, New Zealand." Journal of Clinical Oncology 31, no. 4_suppl (February 1, 2013): 370. http://dx.doi.org/10.1200/jco.2013.31.4_suppl.370.

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370 Background: New Zealand has a high incidence of colorectal cancer; the death rate is the highest amongst developed countries. New Zealand does not have a national screening program for colorectal cancer yet. This study was done in a region with a higher proportion Maori ethnicity. We hypothesized that there are differences in presentation and pathology of colorectal cancer between Maori and European people. Methods: A review of new cases of colorectal cancer presenting over a period of three years (2008-2011) at Whakatane Hospital was done. Data was collected from clinical records and entered into SPSS software. Results: 113 new cases of colorectal cancer were identified. Median age was 73 years. Maori patients were younger than the rest (median age 60 vs 74.5; p < 0.05). 95 patients were of European ethnicity and 15 were Maori. The predominant sign/symptom on presentation was PR bleeding (32%). Only 5 cases were asymptomatic and diagnosed on surveillance colonoscopy. The histologic type of tumor was adenocarcinoma in 111 cases. The most common site of the tumors was the rectum (18.6%). 34.5% cases had localized disease (stage 1, 2A) with no significant difference between Maori and the rest.18.6% cases had distant metastasis with no significant difference between Maori and the rest. Curative surgery was not done in 16 patients due to advanced disease, comorbidities or patient refusal. Conclusions: A higher proportion of patients were diagnosed with localized disease at presentation compared to the rest of New Zealand.. Fewer Maori patients had colorectal cancer in view of the higher proportion of Maori in the area (42-61%). The age of Maori was significantly lower than the rest. Colorectal cancer screening in New Zealand will likely detect cancer earlier. [Table: see text]
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Dissertations / Theses on the topic "Whakatane"

1

Taylor, Susanna K. "A long timescale high-resolution fault activity history of the Whakatane Graben, Bay of Plenty, New Zealand." Thesis, University of Southampton, 2003. https://eprints.soton.ac.uk/427163/.

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The Whakatane Graben is a back-arc basin situated in the Bay of Plenty, North Island, New Zealand, associated with the oblique westward subduction of the Pacific Plate beneath the Australian Plate. The data presented in this thesis reveal both long-term and short-term normal fault behaviour in a fault population surrounding and including one of the most active faults in the offshore graben. Closely spaced (100 - 200 m separation) multichannel seismic and high resolution (chirp sonar, 3.5 kHz and boomer) profiles were collected during cruises in December 1999 and January 2001. These data were processed and interpreted and fault displacement data were extracted. The Rangitaiki Fault lies in the centre of the Whakatane Graben, and is now recognised as a 20 km long, linked, segmented normal fault. The displacement profile of the fully linked Rangitaiki Fault resembles that of a single fault, with a maximum close to the centre and displacements decreasing towards the tips. The fault was found to have initiated as 5 isolated segments, which grew together over 1 Ma. Fault tip propagation was the dominant faulting process initially, followed by the development of relay zones and their subsequent breaching. The system became fully linked between 300 ka and 17 ka, and increased in displacement rate from 0.52 ± 0.18 mm yr⁻¹ prior to linkage, to 1.41 ± 0.31 mm yr⁻¹ afterward. Accurate observations of fault growth rates are hampered by the limited age control of the seismic horizons. The fault propagated northwards and the fault system present today is interpreted as a highly evolved damage zone, where optimally oriented and located faults have linked to form the major Rangitaiki Fault structure and have increased in displacement rate. Displacement is transferred southward from the Rangitaiki Fault onto the newly identified Thornton Fault. The Thornton Fault is along-strike from the onshore surface ruptures caused by the 1987 Edgecumbe earthquake (magnitude 6.3). A repeat time of 320-600 years is inferred for Edgecumbe size events on the Rangitaiki Fault, close to the maximum magnitude for that size of fault. The combined extension rate for all observed faults across the pseudo-3D survey area for the last 17 ± 1 ka is 2.4-3.4 mm yr⁻¹, increased from 0.7-0.9 mm yr⁻¹ for the time interval between 300-17 ka. The increase in extension rate observed in the Whakatane Graben is interpreted as resulting from the eastward migration of the locus of deformation within the Bay of Plenty towards the Hikurangi subduction zone.
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Books on the topic "Whakatane"

1

Beverley, McCulloch, and Wilson John, eds. Unearthing New Zealand. Private Bay: GP Books, 1989.

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2

United Nations. Sub-commission on Prevention of Discrimination and Protection of Minorities. Working Group on Indigenous Populations and International Conference on the Cultural & Intellectual Property Rights of Indigenous Peoples (1st : 1993 : Whakatane, New Zealand)., eds. Mataatua declaration on cultural and intellectual property rights of indigenous peoples, June 1993: First International Conference on the Cultural & Intellectual Property Rights of Indigenous Peoples, Whakatane, 12-18 June 1993, Aotearoa, New Zealand. Geneva: United Nations, 1993.

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3

Maire, Tau Te, ed. Te Whakatau kaupapa: Ngai Tahu resource management strategy for the Canterbury Region. Wellington, N.Z: Aoraki Press, 1990.

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4

New Zealand. Office of the Commissioner for Children., ed. The United Nations Convention on the Rights of the Child =: He hui Whakatau i te mana o te tamaiti a te whakakotahitanga o ngā whenua o te ao. Wellington, N.Z: Office of the Commissioner for Children with the assistance of UNICEF, 1992.

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Book chapters on the topic "Whakatane"

1

Strickson-Pua, Mua. "‘Whakatangi’." In Making Settler Colonial Space, 295–96. London: Palgrave Macmillan UK, 2010. http://dx.doi.org/10.1057/9780230277946_19.

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2

Field, B. D., R. M. Pollock, G. H. Browne, M. Scheihing, and M. Tomasso. "Outcrop Analog Study of Turbidites of the Miocene Whakataki Formation, New Zealand: Significance for Reservoir Volumetrics and Modelling." In Reservoir Characterization: Integrating Technology and Business Practices: 26th Annual, 729–54. SOCIETY OF ECONOMIC PALEONTOLOGISTS AND MINERALOGISTS, 2006. http://dx.doi.org/10.5724/gcs.06.26.0729.

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Journal articles
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