Relevant bibliographies by topics / Taranaki

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  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Taranaki'

Author: Grafiati
Published: 4 June 2021
Last updated: 31 January 2023

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Journal articles on the topic "Taranaki"

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Sissons, Jeffrey. "The Taranaki iconoclasm." Journal of the Polynesian Society 128, no. 4 (December 2019): 373–90. http://dx.doi.org/10.15286/jps.128.4.373-390.

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Naus, Natasha. "The "Taranaki Type": C.H. Moore and the "revolutionary" fresh-air classroom design." Architectural History Aotearoa 8 (September 6, 2021): 36–46. http://dx.doi.org/10.26686/aha.v8i.7099.

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Charles Howard Moore was the Taranaki Education Board Architect from 1920-43. During his tenure Moore developed an open-air classroom design that he called the "Taranaki type"; a design that he claimed was an improvement on the "Fendalton type" of Christchurch. The first Taranaki "fresh air classroom" was opened in New Plymouth in 1928. The "Taranaki type" embraced the principles of natural light and fresh air in an innovative and thoughtful way that took into consideration climatic conditions and the needs of the users. Moore's distinctive design dominated classroom construction throughout the Taranaki region and many of them continue to be used for educational purposes. The New Zealand Historic Places Trust has registered examples of the Taranaki fresh-air classroom and many have been identified by local councils for their architectural and technological values. However, little has been written about CH Moore - his life, training, experiences, and influences. Was he a lone practitioner of the open-air design? Was his design "revolutionary"? Were his classrooms successful? Utilising a variety of archival sources, genealogical research, and comparative analysis, this paper will reveal a more detailed picture of CH Moore and examine his contribution to the design of educational buildings in New Zealand.
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Paterson, Lachy. "Ko Taranaki Te Maunga." Australian Historical Studies 50, no. 4 (October 2, 2019): 536–37. http://dx.doi.org/10.1080/1031461x.2019.1663753.

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Tamaira, Katrina. "Ko Taranaki te Maunga." Archives and Manuscripts 48, no. 3 (March 22, 2020): 353–55. http://dx.doi.org/10.1080/01576895.2020.1732086.

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Sylvester and Mctavish. "Taranaki community partnership model." Journal of Nursing Management 6, no. 2 (March 1998): 71–75. http://dx.doi.org/10.1046/j.1365-2834.1998.00048.x.

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LIU, DONG, and ZHI-QIANG ZHANG. "New Zealand Austrophthiracarus (Acari, Oribatida, Steganacaridae): two new species from the North Island." Zootaxa 4500, no. 3 (October 16, 2018): 443. http://dx.doi.org/10.11646/zootaxa.4500.3.10.

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Two new species of Austrophthiracarus (Oribatida: Steganacaridae) from national parks on the North Island of New Zealand are described: Austrophthiracarus taranaki sp. nov. from moss along tracks in Wilkies Pools, Egmont National Park, Taranaki and Austrophthiracarus whirinaki sp. nov. from litter in Whirinaki Forest, between Rotorua and Taupo. An updated key to all known species of Austrophthiracarus in New Zealand is presented.
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Uruski, C., P. Baillie, and V. Stagpoole. "DEVELOPMENT OF THE TARANAKI BASIN AND COMPARISONS WITH THE GIPPSLAND BASIN: IMPLICATIONS FOR DEEPWATER EXPLORATION." APPEA Journal 43, no. 1 (2003): 185. http://dx.doi.org/10.1071/aj02009.

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Exploration of the Taranaki Basin entered a new phase in 2001 with Astrolabe, a 6,200 km high-quality 2D seismic survey acquired by TGS-NOPEC that has outlined a large depocentre containing up to 10 km of sedimentary fill. This new data has extended the previously-known Taranaki Basin into deeper water beyond the shelf edge. Subsequently, the New Zealand Government released an area of 42,000 km2 for competitive bidding to close in September 2003.Sequence analysis shows that a major deltaic system, comparable to the Golden Beach and Emperor subgroups of the Gippsland Basin, built into a restricted seaway during the Late Cretaceous and culminated with deposition of the Rakopi Formation coal measure succession. The Rakopi Formation covers an area of at least 15,000 km2 of the study area and was followed by a transgression that continued until the Miocene.Minor Eocene folding created broad structures with potential to trap large volumes of petroleum. Other potential trapping structures include drape across Cretaceous rift blocks and turbidite mounds of Miocene age.Modelling shows that much of the Early Cretaceous delta is thermally mature and should be expelling petroleum today. Reservoir facies are present at many horizons, but the primary target is expected to be sandstones of the Rakopi Formation coal measures.Many analogies can be drawn between the Taranaki and Gippsland basins. The deepwater Taranaki basin appears to be equivalent, however, to the offshore, oilprone part of Gippsland while the nearshore Taranaki and Great South basins together form an analogy for the more gas-prone nearshore part of Gippsland.
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Strogen, Dominic P., Karen E. Higgs, Angela G. Griffin, and Hugh E. G. Morgans. "Late Eocene – Early Miocene facies and stratigraphic development, Taranaki Basin, New Zealand: the transition to plate boundary tectonics during regional transgression." Geological Magazine 156, no. 10 (March 11, 2019): 1751–70. http://dx.doi.org/10.1017/s0016756818000997.

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AbstractEight latest Eocene to earliest Miocene stratigraphic surfaces have been identified in petroleum well data from the Taranaki Basin, New Zealand. These surfaces define seven regional sedimentary packages, of variable thickness and lithofacies, forming a mixed siliciclastic–carbonate system. The evolving tectonic setting, particularly the initial development of the Australian–Pacific convergent margin, controlled geographic, stratigraphic and facies variability. This tectonic signal overprinted a regional transgressive trend that culminated in latest Oligocene times. The earliest influence of active compressional tectonics is reflected in the preservation of latest Eocene – Early Oligocene deepwater sediments in the northern Taranaki Basin. Thickness patterns for all mid Oligocene units onwards show a shift in sedimentation to the eastern Taranaki Basin, controlled by reverse movement on the Taranaki Fault System. This resulted in the deposition of a thick sedimentary wedge, initially of coarse clastic sediments, later carbonate dominated, in the foredeep close to the fault. In contrast, Oligocene active normal faulting in a small sub-basin in the south may represent the most northerly evidence for rifting in southern Zealandia, related to Emerald Basin formation. The Early Miocene period saw a return to clastic-dominated deposition, the onset of regional regression and the southward propagation of compressional tectonics.
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Hart, A. W. "NEW ZEALAND’S TARANAKI BASIN: GIANTS IN THE GRABEN?" APPEA Journal 42, no. 1 (2002): 331. http://dx.doi.org/10.1071/aj01018.

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During the past 50 years of utilising modern techniques in New Zealand’s Taranaki Basin, explorers have both been rewarded by its bountiful accumulations and frustrated by its complicated morphology. Numerous superimposed sub-basins, depocentres, areas of uplift, interbedded volcanic edifices and recent volcanism contribute to the complexity of New Zealand’s only producing province. Exploration has been successful along the flanks of the basin, but the time has come to focus on the numerous grabens forming the Taranaki Basin.The basin is a Late Cretaceous rift more than twice the size of the North Sea’s prolific Viking graben, but only 120 wildcats have been drilled since 1955, with only 50 offshore. Horst, tilted fault block, inversion features and thrust anticlines have been the traditional targets, but companies are showing increased interest in relatively more difficult plays involving turbiditic, volcaniclastic and diagenetic reservoirs.The axis of the 6,000 km2 Northern Taranaki graben, the northern part of the Taranaki Basin, has not been penetrated by the drill bit and offers numerous exploration opportunities for basin floor and slope fans of Eocene and Miocene age. Acoustic scattering, diffraction and absorption within a chain of buried Miocene stratovolcanoes inhibit seismic energy from passing into the older sequences, which consist of numerous basin floor fan sequences. Long avoided by exploration programs, volcanic edifices were found to possess good reservoir characteristics and entrap hydrocarbons at Kora–1. The 7000+ km3 of layered extrusive volcanic rock in the graben cannot therefore be discounted as potential reservoir. Another play developed by Miocene magmatism is the doming of potential turbidite reservoirs by underlying igneous feeder dyke systems. In addition, the wells drilled at Kora identified a more elusive play concept—that of potentially large petroleum accumulations stratigraphically trapped downdip from diagenetically altered reservoirs, serving as sealing lithologies, near the igneous feeder dyke systems.As most seismic records in the Northern Taranaki graben were acquired more than a decade ago, modern seismic acquisition and processing technologies are needed to penetrate the buried volcanic edifices and unlock the basin’s story. A better understanding of the basin’s complexities, more cost-effective drilling techniques and a willingness to explore for targets in the source kitchens may finally expose the true potential of the Taranaki Basin.
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Yates, L. J., and M. J. Hedley. "Understanding winter sodium deposition in Taranaki, New Zealand." Soil Research 46, no. 7 (2008): 600. http://dx.doi.org/10.1071/sr07211.

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Research conducted in a limited number of regions has identified that Na deposition rate (kg Na/ha) is strongly influenced by 4 main factors: distance from coast, rainfall, wind speed, and wind direction. Despite the potential importance of Na deposition to the productivity of dairy farms, no comprehensive research has been conducted in Taranaki, New Zealand. Na, K, Ca, and Mg concentrations were determined in weekly rainwater samples collected in standard rain gauges erected at 15 sites, along 4 transects around Taranaki, between May and September 2006. Recorded Na concentrations ranged between 0.40 and 38 mg/L. High Na concentrations were associated with low rainfall volumes and proximity to the coast first receiving the prevailing wind, which was, during this period, the southern Taranaki coast. Na deposition ranged between 0.04 and 25 kg/ha.week. Equations were derived to predict the average Na concentration in rainwater and Na deposition in Taranaki for the 2006 winter period. The most influential factor explaining the variation in average Na concentration was the distance of the collector from the southern coast. Na and Mg depositions were highly correlated (R2 = 0.93; P < 0.01; n = 155), whereas correlations of Na with K or Ca were not as strong (R2 = 0.49 and 0.61, respectively). Measured Na deposition rates exceed those predicted by algorithms used in current nutrient budgeting software and could be used to improve this nutrient management software.
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Dissertations / Theses on the topic "Taranaki"

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Smith, Ailsa Lorraine. "Taranaki waiata tangi and feelings for place." Lincoln University, 2001. http://hdl.handle.net/10182/2137.

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The occupation of Moutoa Gardens in 1995 highlighted efforts by Whanganui iwi to draw attention to the non-settlement of long-standing land grievances arising out of land confiscations by the Crown in New Zealand in the 1860s. Maori attitudes to land have not been well understood by successive New Zealand governments since that time, nor by many Pakeha New Zealanders. In an effort to overcome that lack of understanding, this thesis studies a particular genre of Maori composition; namely, waiata tangi or songs of lament, which contain a strong indigenous sense of place component. The waiata used in this study derive from my tribal area of Taranaki, which is linked historically and through whakapapa with Whanganui iwi. These waiata were recorded in manuscript form in the 1890s by my great-grandfather Te Kahui Kararehe, and are a good source from which to draw conclusions about the traditional nature of Maori feelings for place. Two strands run throughout this thesis. The first examines the nature of Maori feelings for place and land, which have endured through primary socialisation to the present day. By focusing upon a form of expression that reveals the attachment of Maori towards their ancestral homelands, it is hoped that the largely monocultural Pakeha majority in New Zealand will be made aware of that attachment. It is also hoped that Pakeha may be suitably informed of the consequences of colonialist intervention in the affairs of the Maori people since 1840, which have resulted in cultural deprivation and material disadvantage at the present day. In the current climate of government moves to address the problems bequeathed them by their predecessors, it is important that the settlement of land claims and waterways under the Treaty of Waitangi should proceed unhindered by misapprehension and misinformation on the part of the public at large. The second strand of my thesis concerns the waiata texts themselves, which I wish to bring to the attention of the descendants of the composers of those waiata, who may or may not know of their existence. Since so much of value has been lost to the Maori world it is important that the culturally precious items that remain should be restored as soon as possible to those to whom they rightfully belong. Key themes examined in this thesis are the nature of Maori "feelings" for place and a "sense" of place; Maori research methodologies and considerations, including Maori cosmology and genealogical lines of descent; ethical concerns and intellectual property rights; ethnographic writings from the nineteenth century which tried to make sense of Maori imagery and habits of thought; the Kahui Papers from which the waiata were drawn; and the content and imagery of the waiata themselves. I also discuss the use of hermeneutics as a methodological device for unlocking the meanings of words and references in the waiata, and present the results both from a western sense of place perspective and a Maori viewpoint based on cultural concepts and understandings.
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Finnis, Kristen Kay, and n/a. "Resilience and vulnerability in communities around Mt Taranaki." University of Otago. Department of Geology, 2007. http://adt.otago.ac.nz./public/adt-NZDU20070503.100402.

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The aim of this thesis is to examine the resilience and vulnerability of Taranaki communities to volcanic hazards, and to propose a strategy to ensure the safety and longevity of Taranaki residents in the event of an eruption. Mt Taranaki is a dormant volcano that is surrounded by a ring plain populated by over 100,000 people. The volcano has had an average eruptive cycle of 330 years, with the last eruption dated at ~1755 AD. Hazards include ash fall, lahars, debris avalanches and pyroclastic density currents. Inglewood, Stratford and Opunake are the largest population centres located in moderate to high hazard zones, and for this reason were chosen as the study communities. Resilience is defined as the capacity to respond to a hazard event by physically and psychologically recovering, adapting to, or changing to similar or better conditions than those experienced before the event. Vulnerability is defined to be people�s incapacity to cope with a hazardous event as a result of their personal characteristics. A person�s vulnerability and resilience is influenced by demographic variables, socio-cognitive variables and preparedness. Inglewood, Stratford and Opunake adults have good self-efficacy and action-coping use, fair risk perceptions, outcome expectancy and response efficacy, but poor understanding of event timing relative to eruption probability, critical awareness, preparedness and information-seeking intentions and preparedness levels. Preparedness is found to be influenced by residents� intentions to prepare, which in turn are influenced by critical awareness, action-coping and outcome expectancy. Taranaki students have a fair awareness of hazard and knowledge of correct response behaviours to various hazards. Preparedness, in terms of preparedness measures undertaken, emergency plans made and emergency practices in place, is low. Students who have participated in hazard-education programmes have a better knowledge of response behaviours, lower levels of hazard-related fear, and reported higher level of preparedness. Spatial analyses, carried out to determine the geographic distribution of at-risk groups within the study communities, showed that the areas most at-risk tend to be those with the highest population densities. The spatial analysis was not as beneficial as expected, due to small data sets, but did provide some results to be considered as a basis for further research. Effective public education can be achieved when delivered to a set of guidelines, such as providing information regularly through multiple media and sources, ensuring consistent messages, targeting information to at-risk groups and monitoring programme effectiveness. Community capacity building projects decrease aspects of vulnerability and build resilience by working at a local scale and targeting at-risk groups. Psychological preparedness education helps citizens to mentally prepare for an event and should be a component of all projects. The proposed strategy calls for (a) forming partnerships with relevant stakeholders to assist with public education, research, and funding, (b) further research into the characteristics of Taranaki communities and effective public education campaigns, (c) the development and implementation of a public education schedule and projects that build community capacity, and d) long-term planning, periodic revision of programmes and consistent public engagement.
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Keenan, Lauren, and n/a. "Maori perspectives and the Waitangi Tribunal : the 1996 Taranaki report." University of Otago. Department of History, 2005. http://adt.otago.ac.nz./public/adt-NZDU20070504.110209.

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This thesis assesses the extent to which the 1996 Waitangi Tribunal report "Taranaki Report Kaupapa Tuatahi" allowed for and took heed of Maori forms of telling history. In particular, this thesis examines whether the Tribunal reconciles the differences between a Maori perspective and the Western university tradition, or if Maori history is manipulated by the Tribunal process. Due to the nature of the Waitangi Tribunal, as well as its empowering statute, the extent to which it may incorporate the Maori history within its reports is limited, it does not incorporate other means by which Maori tell their histories. The Waitangi Tribunal process, however, has had an unforseen outcome: the compilation and preservation of a fantastic historical primary source detailing Maori history. It is imperative that this resource not go unrecognised, and that these primary sources are able to be accessed by researches with an interest in Taranaki Maori
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Sherburn, Steven. "Structure, seismicity, and tectonics of the Taranaki region, New Zealand." Thesis, University of Cambridge, 2005. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.614757.

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Chenrai, Piyaphong. "Seismic stratigraphy and fluid flow in the Taranaki and Great South Basins, offshore New Zealand." Thesis, University of Manchester, 2016. https://www.research.manchester.ac.uk/portal/en/theses/seismic-stratigraphy-and-fluid-flow-in-the-taranaki-and-great-south-basins-offshore-new-zealand(433b3426-c261-4e29-97fd-8bd8478728a5).html.

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This study utilises seismic data to improve understanding of the subsurface fluid flow behaviour in the Taranaki and Great South Basins offshore New Zealand. The aim of this study is to characterise fluid flow features and to investigate their genesis, fluid origins and implications for subsurface fluid plumbing system by integrating seismic interpretation and 3D petroleum systems modelling techniques. After an early phase studying Pliocene pockmarks in the Taranaki Basin, this study has been focused on the subsurface fluid plumbing system and on the fluid expulsion history in the Great South Basin. The Taranaki Basin lies on the west coast and offshore of the North Island, New Zealand. The seismic interpretation revealed that paleo-pockmark formation in the study area relates to fluid escape due to a rapid sediment loading environment in a distal fan setting. Seismic analysis rules out any links between the paleo-pockmarks and faulting. The relationship between paleo-pockmark occurrence and fan depositional thickness variations suggests that pore-water expulsion during overburden progradation is the most likely cause of the paleo-pockmarks. The rapid sediment loading generated overpressure which was greatest on the proximal fan due to a lateral gradient in overburden pressure. Fluids were consequently forced towards the fan distal parts where, eventually, the pore pressure exceeded the fracture gradient of the seal. The Great South Basin lies off the southern coast of the South Island of New Zealand and is located beneath the modern shelf area. Evidence for past and present subsurface fluid flow in this basin is manifested by the presence of numerous paleo-pockmarks, seabed pockmarks, polygonal fault systems, bright spots and bottom simulating reflections (BSR), all of which help constrain aspects of the overburden plumbing system and may provide clues to deeper hydrocarbon prospectivity in this frontier region. The various types of fluid flow features observed in this study are interpreted to be caused by different fluid origins and mechanisms based on evidences from seismic interpretation in the study area. The possible fluid origins which contribute to fluid flow features in the Great South Basin are compactional pore water as well as biogenic and thermogenic hydrocarbons. Using 3D seismic attribute analysis it was possible to highlight the occurrence of these features, particularly polygonal faults and pockmarks, which tend to be hosted within fine-grained sequences. Paleo- and present-day fluid flow features were investigated using 3D basin and petroleum systems modelling with varying heat flow scenarios. The models predict that thermogenic gas is currently being generated in mid-Cretaceous sedimentary sequences and possibly migrates along tectonic faults and polygonal faults feeding present-day pockmarks at the seabed. The models suggest that biogenic gas was the main fluid source for the Middle Eocene paleo-pockmarks and compactional pore fluid may be the main fluid contributor to the Late Eocene paleo-pockmarks. Different heat flow scenarios show that only mid-Cretaceous source rocks have reached thermal maturity in the basin, whilst Late Cretaceous and Paleocene source rocks would be largely immature. The observations and interpretations provided here contribute to the ongoing discussion on basin de-watering and de-gassing and the fluid contributors involved in pockmark formation and the use of pockmarks as a potential indicator of hydrocarbon expulsion. It is clear from this study that seismically-defined fluid flow features should be integrated into petroleum systems modelling of frontier and mature exploration areas in order to improve our understanding on fluid phases, their migration routes, timings and eventual expulsion history.
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Amansure, Giovanni Ricardo. "Source rock characterization of the organic rich intervals of the Taranaki Basin, Offshore New Zealand." University of the Western Cape, 2015. http://hdl.handle.net/11394/5057.

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>Magister Scientiae - MSc
The Taranaki Basin is a large (ca. 330,000 km²) sedimentary basin found along the west coast of the northern island of New Zealand. The basin lies partly onshore but mostly offshore below the broad continental shelf to the west of central North Island. The Taranaki Basin is the first sedimentary basin to be explored in New Zealand and is currently New Zealand’s only hydrocarbon producing basin, with approximately 418 million barrels (MMbbl) of oil and 6190 billion cubic feet (bcf) of gas produced by the end of 2011. Most of New Zealand’s known oil and gas accumulations are geochemically typed to coaly facies of Late Cretaceous and Paleogene ages. The main objective of this thesis is to characterize the source rock quality of the organic rich intervals of the Taranaki Basin, namely, the Wainui Member of the North Cape Formation and the Rakopi Formation. The Rakopi Formation comprises terrestrially deposited coal measures, while the North Cape Formation is generally composed of marine rocks. These Formations make up the Pakawau Group. The objective will be achieved using two key methods. Firstly, the derivation of TOC logs using Passey’s log overlay method (Passey et al., 1990) and secondly, the generation of source rock quality maps (i.e. source rock richness mapping and source potential index mapping). This will integrate concepts relating to petrophysical wireline logs, seismic interpretation, core log information, geochemical analysis, depth mapping and isopach mapping. The results obtained from this study confirms the petroleum potential of the organic rich intervals of the Taranaki Basin. Using Passey’s method it was shown that excellent average percent TOC values are encountered for both the Wainui Member of the North Cape Formation and the Rakopi Formation. From source potential index mapping, it can be concluded that the Rakopi formation has a high source potential index (>1000SPI) on the continental shelf, which indicates that it has excellent potential for petroleum generation. The Wainui Member however, shows less potential for petroleum generation on the shelf, this being attributed to generally low net thicknesses on the shelf.
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Goldsmith, Steven Todd. "Geochemical Fluxes and Weathering on High Standing Islands: Taranaki and Manawatu-Wanganui Regions New Zealand." The Ohio State University, 2005. http://rave.ohiolink.edu/etdc/view?acc_num=osu1391601668.

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Boulton, Leanne. "Native reserves, assimilation and self-determination : Te Atiawa, the Crown and settlers, North Taranaki 1840-1875." Thesis, University of Canterbury. History, 2004. http://hdl.handle.net/10092/1995.

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The historiography of Native reserves which has emerged from the Waitangi Tribunal’s historical inquiry into Maori grievances against the Crown since 1985 has necessarily been preoccupied with the creation and alienation of reserves in the context of the Crown-iwi partnership and national Native reserve policies. This thesis investigates the local dimensions of Crown policy and restores a focus on Crown-hapu relations by offering an analysis of the creation, utilisation and administration of the Native reserves of the FitzRoy, Omata, Grey, Waiwakaiho and Hua blocks in North Taranaki between 1840 and 1875. It argues that Native reserve were intended to contain, control and assimilate Maori and as such the Native reserve policies of the New Zealand Company and the Crown were indicative of visions of the Maori future within an evolving Anglo-settler society. Although this agenda of assimilation remained prominent, the views of Crown officials regarding how Native reserves would perform these functions changed markedly between the 1840s and 1850s. In particular there was a shift away from scattering reserves amongst settler sections in the hope that Maori would emulate settlers and learn to be “civilised” to an attempt to have Maori re-purchasing land from the Crown instead of Native reserves, which they would hold in individualised Crown title. Thus it was hoped that the communal nature of Maori society would be broken down and Maori would come to adhere to British social, legal and economic norms. At the same time this thesis recovers and assesses the world-views and expectations of Te Atiawa hapu about their future with Pakeha. It demonstrates the impact of these visions on hapu understandings of the purpose and nature of Native reserves, and on the ways in they formed economic and social relationships with settlers in utilised the reserves. The combination of primary historical sources and a statistical analysis demonstrates that these relationships played a significant role in shaping the work of the Native reserves commissioners appointed under New Zealand Native Reserves Act 1856 in Taranaki. In particular they lead to the commissioners modifying their initial pro-active approach to bringing the reserves under their administration if favour of acting as intermediaries between Te Atiawa and settlers with pre-arranged leases. A comparison of the nature and utilisation of reserves in hapu and Crown control demonstrates that although Te Atiawa retained control of approximately half of the Native reserves in these blocks all of their most commercially viable reserves were brought under the Act, and in the process the Native title was extinguished. Co-operative relationships, which underpinned the leasing of reserves in the private sphere, were in marked contrast to public settler expressions of unease about Te Atiawa and their reserves in New Plymouth, and to mistrust between the two communities that reached its zenith during the Taranaki Wars. Such mistrust ultimately lead to the absence of Te Atiawa Native reserves and communities from the city of New Plymouth.
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Cammans, Phillip C. "Mechanisms and Timing of Pluton Emplacement in Taranaki Basin, New Zealand Using Three-Dimensional Seismic Analysis." BYU ScholarsArchive, 2015. https://scholarsarchive.byu.edu/etd/5649.

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Several off-shore volcano-plutonic complexes are imaged in detail in the Parihaka 3D seismic survey in the Taranaki Basin of New Zealand. Three intrusions were analyzed for this study. Part of the Mohakatino Volcanic Centre (15 to 1.6 Ma), these intrusions have steep sides, no resolvable base reflectors, no internal stratification or structure, and they exhibit doming and faulting in the sedimentary strata above the intrusions. Deformation along the sides is dominated by highly attenuated, dipping strata with dips of 45° or higher that decrease rapidly away from the intrusions. Doming extends several hundred meters from the margins and produced many high-angle normal faults and thinned strata. The intrusions lie near normal faults with the Northern Intrusion lying directly adjacent to a segment of the Parihaka Fault. The Central Intrusion has localized normal faults cutting a graben in the area directly above the intrusion and extending in a NE-SW direction away from it. The Western Intrusion is near the western edge of the Parihaka 3D dataset and is not situated directly adjacent to extensional faults.Two distinct zones of intrusion-related faults developed around both the Northern and Central Intrusions representing two different stress regimes present during emplacement, a local stress field created by the intrusions during emplacement and the regional stress field. The deeper zones contain short radial faults that extend away from the intrusion in all directions, representing a local stress field. The shallower faults have a radial pattern above the apex of each intrusion, but farther from it, they follow the regional stress field and trend NE. Using our techniques to interpret radial faulting above both intrusions and the principal of cross-cutting relations, timing of emplacement for these intrusions are 3.5 Ma for the Northern Intrusion and between 5 and 4 Ma for the Central and Western Intrusions.Observed space-making mechanisms for the Northern and Central Intrusions include doming (~16% and 11%, respectively), thinning and extension of roof strata (~4% for both), and extension within the basin itself (29% and 12%). Stoping and floor subsidence may have occurred, but are not visible in the seismic images. Magmatic extension may have played a significant role in emplacement.Several gas-rich zones are also imaged within the seismic data near the sea-floor. They appear as areas of acoustic impedance reversal compared to surrounding sedimentary strata and have a reversal of amplitude when compared to the sea floor. The gas in these zones is either biogenic or sourced from deeper reservoirs cut by normal faults.
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Hopcroft, Bradley Scott. "Lithology and provenance of late Eocene - Oligocene sediments in eastern Taranaki Basin margin and implications for paleogeography." The University of Waikato, 2009. http://hdl.handle.net/10289/2793.

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The latest Eocene and Oligocene was a time of marked paleoenvironmental change in Taranaki Basin, involving a transition from the accumulation of coal measures and inner shelf deposits to the development of upper bathyal environments. Up until the end of the Early Oligocene (Lower Whaingaroan Stage) Taranaki Basin had an extensional tectonic setting. Marine transgression culminated in the accumulation of condensed facies of the Matapo Sandstone Member of the lower part of the Ngatoro Group. During the Late Oligocene (Upper Whaingaroan Stage) Taranaki Basin's tectonic setting changed to one of crustal shortening with basement overthrusting westward into the basin on Taranaki Fault. The major part of the Ngatoro Group in thickness, including the Tariki Sandstone Member, Otaraoa Formation, Tikorangi Formation and Taimana Formation, accumulated in response to this change in tectonic setting. Various methods of stratigraphic and sedimentological characterisation have been undertaken to evaluate the stratigraphy of the Ngatoro Group. Wireline log records have been calibrated through particle sizing and carbonate digestion of well cuttings. A suite of wireline motifs have been defined for formations and members of the Ngatoro Group. The integration with other lithological and paleoenvironmental data sources has helped to better define the Late Eocene - Oligocene stratigraphy and sedimentary facies for eastern Taranaki Basin margin. U-Pb geochronology by laser ablation inductively coupled plasma-mass spectrometry (LA-ICP-MS) has been used to determine detrital ages for over 350 zircons from 13 samples of Late Eocene - Oligocene sandstone samples in eastern Taranaki Basin and correlative onshore North Island units. The spread of ages (1554 - 102 Ma) and the proportion of ages in particular age bands integrated with modal petrography data have aided provenance evaluation. A range of source rocks contributed to the Late Eocene - Oligocene sedimentary units analysed, mainly the Waipapa Terrane (Early Permian to Late Jurassic) as shown by 206Pb/238U zircon ages and the abundance of fine-grained sedimentary rock fragments observed in samples. The Median Batholith (i.e. Darran/Median Suite and Separation Point Suite) is also identified as a significant source, indicated by Early Triassic to Early Jurassic and Early Cretaceous 206Pb/238U zircon ages and an abundance of quartz in samples. Other minor sources identified include Murihiku and Caples Terranes, Rakaia Sub-terrane and possibly the Karamea Batholith. The Tariki Sandstone and the Hauturu Sandstone have the same source, with the main 206Pb/238U zircon ages of aggregated samples (124 - 116 Ma and 121 Ma, respectively) consistent with a Separation Point Suite/Median Batholith (124 - 116 Ma) source. Derivation of sediments from a landmass that existed to the east and southeast of the Wellington area has been inferred for the Late Eocene - Oligocene units, with subsequent migration of sediments northward into Taranaki Basin and the Waikato Region (i.e. Te Kuiti Group depocentre) via longshore drift. New provenance data have been used to revise understanding about the development of eastern Taranaki Basin margin through the Late Eocene to earliest Miocene. Three new paleogeography maps are presented for the Runangan (Late Eocene), Lower Whaingaroan (Early Oligocene) and Upper Whaingaroan (early-mid-Oligocene). New paleogeography interpretations illustrate a dramatic change in the basin development between Matapo Sandstone (Lower Whaingaroan) and Tariki Sandstone (Upper Whaingaroan) deposition, consistent with an Upper Whaingaroan age for the start of reverse movement on Taranaki Fault.
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Books on the topic "Taranaki"

1

Gail, Henry, and Henry Gail, eds. Taranaki: An illustrated history. Auckland, N.Z: Reed Books, 2000.

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Moorhead, Murray. Tales of old North Taranaki. [New Plymouth, N.Z.?: Published by the author in association with the Taranaki Branch, NZ Founders Society, 1991.

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Houston, John. Maori life in old Taranaki. 2nd ed. Auckland: Reed Books, 2006.

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Prickett, Nigel. Historic Taranaki: An archaeological guide. Wellington: GP Books, 1990.

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Riseborough, Hazel. Days of darkness: Taranaki, 1878-1884. Wellington, N.Z: Allen & Unwin New Zealand in associatio n with the Port Nicholson Press, 1989.

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Tucker, Rob. Taranaki: A journey from the heart. 6th ed. New Plymouth, [N.Z.]: Tucker Media, 2014.

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Anthony, Walton. Archaeology of the Taranaki-Wanganui region. Wellington, N.Z: Dept. of Conservation, 2001.

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Riseborough, Hazel. Days of darkness: Taranaki, 1878-1884. Auckland, N.Z: Penguin Books, 2002.

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Port Taranaki: 115 years of elected control. New Plymouth, N.Z.]: Westgate Transport, 1991.

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Johnston, Kerensa. He iti, he taonga: Taranaki Māori women speak. [Ohope, N.Z: Kerensa Johnston], 2008.

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Book chapters on the topic "Taranaki"

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Armstrong, Phillip A., and David S. Chapman. "Combining Tectonics and Thermal Fields in Taranaki Basin, New Zealand." In Computer Applications in the Earth Sciences, 151–76. Boston, MA: Springer US, 1999. http://dx.doi.org/10.1007/978-1-4615-4751-8_8.

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Omeru, Tuviere, Joseph A. Cartwright, and Suzanne Bull. "Kinematics of Submarine Slope Failures in the Deepwater Taranaki Basin, New Zealand." In Submarine Mass Movements and their Consequences, 61–70. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-20979-1_6.

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Procter, Jonathan N., Anke V. Zernack, and Shane J. Cronin. "Computer Simulation of a Volcanic Debris Avalanche from Mt. Taranaki, New Zealand." In Volcanic Debris Avalanches, 281–310. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-57411-6_11.

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Zernack, Anke V. "Volcanic Debris-Avalanche Deposits in the Context of Volcaniclastic Ring Plain Successions—A Case Study from Mt. Taranaki." In Volcanic Debris Avalanches, 211–54. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-57411-6_9.

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O'Malley, Vincent. "Taranaki, 1860-64." In Voices from the New Zealand Wars | He Reo nō ngā Pakanga o Aotearoa, 103–42. Bridget Williams Books, 2021. http://dx.doi.org/10.7810/9781988587790_4.

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Buchanan, Rachel. "Ko Taranaki Te Maunga." In Ko Taranaki Te Maunga, 126–34. Bridget Williams Books, 2018. http://dx.doi.org/10.7810/9781988545288_6.

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Buchanan, Rachel. "Time zones." In Ko Taranaki Te Maunga, 7–23. Bridget Williams Books, 2018. http://dx.doi.org/10.7810/9781988545288_1.

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Buchanan, Rachel. "Paper mountain." In Ko Taranaki Te Maunga, 24–52. Bridget Williams Books, 2018. http://dx.doi.org/10.7810/9781988545288_2.

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Buchanan, Rachel. "The very long sorry." In Ko Taranaki Te Maunga, 53–74. Bridget Williams Books, 2018. http://dx.doi.org/10.7810/9781988545288_3.

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Buchanan, Rachel. "Beating shame." In Ko Taranaki Te Maunga, 75–103. Bridget Williams Books, 2018. http://dx.doi.org/10.7810/9781988545288_4.

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Conference papers on the topic "Taranaki"

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Bull*, Suzanne, Matt G. Hill, Malcolm J. Arnot, Hannu Seebeck, Cathal Reilly, Hai Zhu, and Karsten F. Kroeger. "A Regional Model for New Zealand's Taranaki Basin: The 4-D Taranaki Project." In International Conference and Exhibition, Melbourne, Australia 13-16 September 2015. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2015. http://dx.doi.org/10.1190/ice2015-2210542.

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D'Mello, Nessa, Teresa Ubide Garralda, Georg Florian Zellmer, Jonathan Procter, Gabor Kereszturi, and John Caulfield. "Crystal Stratigraphy of Taranaki Lavas, New Zealand." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.506.

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Adam, John, Shane Cronin, Tracy Rushmer, and Simon Turner. "Petrological Evolution of Mt Taranaki, New Zealand." In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.11824.

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Leitner, B., A. Hart, and G. Thrasher. "Exploration of Igneous Cored Domes, Taranaki Basin, New Zealand." In 63rd EAGE Conference & Exhibition. European Association of Geoscientists & Engineers, 2001. http://dx.doi.org/10.3997/2214-4609-pdb.15.p021.

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Titenko, I., and I. Virshylo. "Burial History Modeling of the Taranaki Basin (New Zealand)." In 15th EAGE International Conference on Geoinformatics - Theoretical and Applied Aspects. Netherlands: EAGE Publications BV, 2016. http://dx.doi.org/10.3997/2214-4609.201600498.

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El Gandy, Eman Ahmed Ibrahiem. "Parihaka Reservoir Characterization by Integrating Well and Seismic Data through Seismic Inversion and Multiattribute Analysis." In International Petroleum Technology Conference. IPTC, 2022. http://dx.doi.org/10.2523/iptc-21945-ms.

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Abstract A geophysical study to understand and Identify Pliocene - Pleistocene channels system and improve better understand of the channel geometry, fill lithology and connectivity and Generate rock property volume, Enhance reservoir quality, Hydrocarbon distribution and sweet spot detection with min. risk in Miocene reservoir (Moki formation). The Taranaki Basin is the only New Zealand basin to produce commercial quantities of hydrocarbons and still being underexplored. The Parihaka field is on the north-western Taranaki Peninsula located along the west coast of New Zealand's North Island (Veritas, 2005) which there only dry hole drilled based on 2D lines (Arawa-1). Moki formation is our main reservoir its depositional environment is turbiditic fan complex. Hydrocarbons are yet to be commercially produced from the Moki Formation on onshore Taranaki, (Smale et al., 1999). There was AVO study called "Investigation of the Miocene Moki Formation Within the Parahaki 3D Survey; Taranaki Basin, Offshore New Zealand Using Some Geophysical Tools" in Moki reservoir to Investigate and assess the AVO response of the Moki sand formation. By using the results of The AVO study, the inversion can apply in the area to enhance the result, generate rock property volume, Enhance reservoir quality, Hydrocarbon distribution and sweet spot detection with min. risk. By running three volumes of post stack inversion (vp, vs, density) and use λ, μ and vp/vs to identify the hydrocarbon contact distribution. Then by using AVO Inversion (Another different fast technic in the relative domain) to prove the results and using Extend Elastic Impedance Method. The result of this study is there are three prospects in Moki formation, the maps show that Arawa -1 at very low probability of hydrocarbon content which provide our result as it is a dry hole. By using multi-Attribute analysis, we can find new channels system in Pliocene age. Depending on the complexity of the channel system, different attribute analyses had varying success with each system. By using 3D curvature, variance and RMS Amplitude we can improve understanding of the Pliocene channel elements in terms of structure, channel evolution, and lithology. Based on the previous results for these channel systems, RMS amplitude and sweetness attributes can use to detect lithological changes that highlight both shale and sand dominant regions of the channel. These results suggest that the lithology of the small channel is refer to the delta lithology in this individuals channel area, and we can interpret the small channel is filled with a sand lithology, which allows the RMS and sweetness to detect in against the mud rich background lithology.
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Uzcátegui*, Marjosbet, Wai Tin Vincent Kong, and Andrea Paxton. "North Taranaki Basin Potential Evaluation Using AVO and Seismic Attributes." In International Conference and Exhibition, Melbourne, Australia 13-16 September 2015. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2015. http://dx.doi.org/10.1190/ice2015-2211529.

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Kalid, Nur Zulfa Abdul, and Umar Hamzah. "Sequence stratigraphy of the Miocene, Pohokura field, Taranaki Basin, New Zealand." In THE 2014 UKM FST POSTGRADUATE COLLOQUIUM: Proceedings of the Universiti Kebangsaan Malaysia, Faculty of Science and Technology 2014 Postgraduate Colloquium. AIP Publishing LLC, 2014. http://dx.doi.org/10.1063/1.4895277.

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Almasgari, Abd Alsalam Abduh Saeed, and Umar Hamzah. "Sequence stratigraphy of the pliocene deposits, Central Taranaki Basin, New Zealand." In THE 2016 UKM FST POSTGRADUATE COLLOQUIUM: Proceedings of the Universiti Kebangsaan Malaysia, Faculty of Science and Technology 2016 Postgraduate Colloquium. Author(s), 2016. http://dx.doi.org/10.1063/1.4966839.

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Smith, Zachary Daniel, Corey Brazell, and Megan Pickard. "CHEMICAL ANALYSIS ON VOLCANICLASTIC DEPOSITS FROM THE TARANAKI BASIN, NEW ZEALAND." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-285011.

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