title: Rapid progradation of the Pliocene-Pleistocene continental margin, northern Taranaki Basin, New Zealand, and implications

authors: Hansen, Rochelle J.

subjects: Taranaki Basin

abstract: Progradation and aggradation of the modern continental margin in northern Taranaki Basin has resulted in the deposition of a thick and rapidly accumulated Pliocene-Pleistocene sedimentary succession. It includes the predominantly muddy Giant Foresets Formation, and the underlying sandy Mangaa Formation. Investigation of the internal attributes and depositional systems associated with the Giant Foresets Formation suggests that it would provide very little effective reservoir for hydrocarbon accumulations, although it does provide essential seal and overburden properties. While the sand-dominated Mangaa Formation could be a hydrocarbon reservoir, drilling so far has yet to reveal any significant hydrocarbon shows. Undoubtedly the most significant contribution that the Giant Foresets and Mangaa Formations have had on petroleum systems in northern Taranaki Basin is the cumulative effect that rapid and substantial accumulation has had on maturation and migration of hydrocarbons in the underlying formations.
Palinspastic restoration of a seismic reflection profile across the Northern Graben, together with isopach mapping of stratigraphic section for biostratigraphic stages, indicates that the thickest part of the Pliocene-Pleistocene succession is along the central axis of the Northern Graben. Deposition of this succession contributed substantially to subsidence within the graben, providing further accommodation for sediment accumulation. Isopach and structure contour maps also reveal the extent to which submarine volcanic massifs were exposed along the axis of the graben and the timing of movement on major faults.

text: Rapid progradation of the Pliocene-Pleistocene continental margin, northern Taranaki Basin, New Zealand, and implications Progradation and aggradation of the modern continental margin in northern Taranaki Basin has resulted in the deposition of a thick and rapidly accumulated Pliocene-Pleistocene sedimentary succession. It includes the predominantly muddy Giant Foresets Formation, and the underlying sandy Mangaa Formation. Investigation of the internal attributes and depositional systems associated with the Giant Foresets Formation suggests that it would provide very little effective reservoir for hydrocarbon accumulations, although it does provide essential seal and overburden properties. While the sand-dominated Mangaa Formation could be a hydrocarbon reservoir, drilling so far has yet to reveal any significant hydrocarbon shows. Undoubtedly the most significant contribution that the Giant Foresets and Mangaa Formations have had on petroleum systems in northern Taranaki Basin is the cumulative effect that rapid and substantial accumulation has had on maturation and migration of hydrocarbons in the underlying formations.
Palinspastic restoration of a seismic reflection profile across the Northern Graben, together with isopach mapping of stratigraphic section for biostratigraphic stages, indicates that the thickest part of the Pliocene-Pleistocene succession is along the central axis of the Northern Graben. Deposition of this succession contributed substantially to subsidence within the graben, providing further accommodation for sediment accumulation. Isopach and structure contour maps also reveal the extent to which submarine volcanic massifs were exposed along the axis of the graben and the timing of movement on major faults.

year: 2004

title: Exuberance in British share prices during the railway mania of the 1840s: Evidence from the Phillips, Shi and Yu Test

authors: Oxley, Les

subjects: explosive behaviour

abstract: In this study, we empirically investigate evidence of explosive behaviour in the British share prices of canals, railways and waterworks in the nineteenth century using the right-tailed unit root test of Phillips, Shi and Yu (2015, PSY). Of particular interest to the Railway Mania in the 1840s, our results provide evidence of exuberance in share prices of railways during the most remarkable events in history. In addition, we find signs of exuberance in canals and waterworks share prices. Our findings will be of great interest to both economic historians and scholars who are interested in the rage of speculation in historical share prices during the Railway Mania

text: Exuberance in British share prices during the railway mania of the 1840s: Evidence from the Phillips, Shi and Yu Test In this study, we empirically investigate evidence of explosive behaviour in the British share prices of canals, railways and waterworks in the nineteenth century using the right-tailed unit root test of Phillips, Shi and Yu (2015, PSY). Of particular interest to the Railway Mania in the 1840s, our results provide evidence of exuberance in share prices of railways during the most remarkable events in history. In addition, we find signs of exuberance in canals and waterworks share prices. Our findings will be of great interest to both economic historians and scholars who are interested in the rage of speculation in historical share prices during the Railway Mania

year: 2017-04

title: Renewal and resistance: Moko in contemporary New Zealand

authors: Nikora, Linda Waimarie

subjects: maori

abstract: Moko is still here, contrary to the widely held belief that the art and custom of moko-Maori skin adornment-had vanished from New Zealand communities. Over the last two decades an increasingly visible number of Maori have revived and renewed the practice, taking colour into their skin. As an indigenous people, re-taking moko confronts and refutes the myth of a 'dying race'. It calls on Maori to recommit to strong Maori identities, customs and traditions and challenges the viewer to re-examine their social representations of moko and moko wearers. This paper reports the resistance strategies of a group of 83 moko wearers. Strategies include (1) educating, representing and reconstructing; (2) invalidating and minimizing representations; (3) building and enhancing social networks; and (4) securing cultural identity and pride. They reflect the celebration of cultural resilience.

text: Renewal and resistance: Moko in contemporary New Zealand Moko is still here, contrary to the widely held belief that the art and custom of moko-Maori skin adornment-had vanished from New Zealand communities. Over the last two decades an increasingly visible number of Maori have revived and renewed the practice, taking colour into their skin. As an indigenous people, re-taking moko confronts and refutes the myth of a 'dying race'. It calls on Maori to recommit to strong Maori identities, customs and traditions and challenges the viewer to re-examine their social representations of moko and moko wearers. This paper reports the resistance strategies of a group of 83 moko wearers. Strategies include (1) educating, representing and reconstructing; (2) invalidating and minimizing representations; (3) building and enhancing social networks; and (4) securing cultural identity and pride. They reflect the celebration of cultural resilience.

year: 2007