title: Theft in the digital: Can you steal virtual property?

authors: Rumbles, Wayne

abstract: This article explores issues arising around the theft of virtual property. It first explains a number of perhaps counter intuitive concepts vital to the understanding of the importance of extending ‘real world’ criminal law and criminal liability to conduct inside virtual worlds such as World of Warcraft or Second Life. This article focuses on theft of virtual property and explores how other jurisdictions are developing responses to this issue. It then develops an analysis of the operation of ‘real world’ New Zealand criminal law rules around theft, in the context of the evolution of virtual property.

text: Theft in the digital: Can you steal virtual property? This article explores issues arising around the theft of virtual property. It first explains a number of perhaps counter intuitive concepts vital to the understanding of the importance of extending ‘real world’ criminal law and criminal liability to conduct inside virtual worlds such as World of Warcraft or Second Life. This article focuses on theft of virtual property and explores how other jurisdictions are developing responses to this issue. It then develops an analysis of the operation of ‘real world’ New Zealand criminal law rules around theft, in the context of the evolution of virtual property.

year: 2011

title: Lithostratigraphy and depositional episodes of the Oligocene carbonate-rich Tikorangi Formation, Taranaki Basin, New Zealand

authors: Hood, Steven D.

subjects: carbonate

abstract: The subsurface Oligocene Tikorangi Formation is a unique and important oil producer in the onshore Waihapa-Ngaere Field, Taranaki Basin, being the only carbonate and fracture-producing reservoir within the basin. Core sample data from seven onshore wells (foredeep megafacies) and a single offshore well (basinal megafacies) are correlated with a suite of sonic and gamma-ray geophysical well log data to derive interpretative carbonate facies for the Tikorangi Formation. Four mixed siliciclastic-carbonate to carbonate facies have been defined: facies A-calcareous siliciclastite (<25% carbonate); facies B-very calcareous siliciclastite (25-50% carbonate); facies C-muddy limestone (50-75% carbonate); and facies D-coarse limestone (>75% carbonate). Single or interbedded combinations of these facies form the basis for identifying nine major lithostratigraphic units in the Tikorangi Formation that are correlatable between the eight wells in this study.The Tikorangi Formation accumulated across a shelf-slope-basin margin within a tectonically diversified basin setting, notably involving considerable off-shelf redeposition of sediment into a bounding foredeep. Analysis of gamma, sonic, and resistivity well logs identifies five major episodes of sedimentary evolution. Episode I comprises retrogradational siliciclastic-dominated redeposited units associated with foredeep subsidence. Episode II is a continuation of episode I retrogradation, but with increased mass-redeposited carbonate influx during accelerated foredeep subsidence and relative sea-level rise, the top marking the maximum flooding surface. Episode III involves a progradational sequence comprising relatively pure redeposited carbonate units associated with declining subsidence rates and minimal siliciclastic input, with movement of facies belts basinward. Episode IV consists of prograding aggradation involving essentially static facies belts dominated by often thick, periodically mass-emplaced, carbonate-rich units separated by thin background siliciclastic shale-like units. Episode V is a retrogradational sequence marking the reintroduction of siliciclastic material into the basin following uplift of Mesozoic basement associated with accelerated compressional tectonics along the Australia-Pacific plate boundary, initially diluting and ultimately extinguishing carbonate production factories and terminating deposition of the Tikorangi Formation.

text: Lithostratigraphy and depositional episodes of the Oligocene carbonate-rich Tikorangi Formation, Taranaki Basin, New Zealand The subsurface Oligocene Tikorangi Formation is a unique and important oil producer in the onshore Waihapa-Ngaere Field, Taranaki Basin, being the only carbonate and fracture-producing reservoir within the basin. Core sample data from seven onshore wells (foredeep megafacies) and a single offshore well (basinal megafacies) are correlated with a suite of sonic and gamma-ray geophysical well log data to derive interpretative carbonate facies for the Tikorangi Formation. Four mixed siliciclastic-carbonate to carbonate facies have been defined: facies A-calcareous siliciclastite (<25% carbonate); facies B-very calcareous siliciclastite (25-50% carbonate); facies C-muddy limestone (50-75% carbonate); and facies D-coarse limestone (>75% carbonate). Single or interbedded combinations of these facies form the basis for identifying nine major lithostratigraphic units in the Tikorangi Formation that are correlatable between the eight wells in this study.The Tikorangi Formation accumulated across a shelf-slope-basin margin within a tectonically diversified basin setting, notably involving considerable off-shelf redeposition of sediment into a bounding foredeep. Analysis of gamma, sonic, and resistivity well logs identifies five major episodes of sedimentary evolution. Episode I comprises retrogradational siliciclastic-dominated redeposited units associated with foredeep subsidence. Episode II is a continuation of episode I retrogradation, but with increased mass-redeposited carbonate influx during accelerated foredeep subsidence and relative sea-level rise, the top marking the maximum flooding surface. Episode III involves a progradational sequence comprising relatively pure redeposited carbonate units associated with declining subsidence rates and minimal siliciclastic input, with movement of facies belts basinward. Episode IV consists of prograding aggradation involving essentially static facies belts dominated by often thick, periodically mass-emplaced, carbonate-rich units separated by thin background siliciclastic shale-like units. Episode V is a retrogradational sequence marking the reintroduction of siliciclastic material into the basin following uplift of Mesozoic basement associated with accelerated compressional tectonics along the Australia-Pacific plate boundary, initially diluting and ultimately extinguishing carbonate production factories and terminating deposition of the Tikorangi Formation.

year: 2003

title: Te mana o te wahine: Young mothers healthcare experiences in pregnancy, birth, and into motherhood

authors: Kolo, Mia Elaine

subjects: Health

abstract: In Aotearoa-New Zealand being a young mother is often associated with clinical and societal ‘risks.’ Younger women have higher rates of maternal depression and suicide, complications during birth, and their babies are more likely to be born preterm, and of smaller gestational age and weight (Perinatal and Maternal Mortality Review Committee, 2012; Te Whatu Ora - Health New Zealand, 2023b, 2023a). Research also indicates that young mothers experience stigmatisation and discrimination that they attribute to their age and/or ethnicity (Adcock, 2016; Makowharemahihi et al., 2014; Rawiri, 2007; Ware, 2019).
In discussion with researchers, discrimination was the topic that young mothers at He Puaawai Teen Parent Centre wanted to talk about. They shared a strong desire to see change in the way that doctors, nurses, and midwives service young parents and were passionate about ensuring that future young mothers had more support. Thus, in responding to their call, 22 parents, including two fathers attending (or recent school-leavers of) He Puaawai Teen Parent Centre volunteered to participate in this study. This qualitative kaupapa Māori study employed a series of wānanga, individual kōrero, and an investigator-triangulation thematic analysis. The research questions explored both the positive and negative healthcare experiences of this cohort during pregnancy, birth, and into motherhood.
The aim of this study was to listen and learn about the experiences of these young parents and co-design informational and/or educational materials to help healthcare practitioners better understand and support young mothers/parents. To spread awareness of the experiences of these young parents, the co-design materials and findings of this study were disseminated via various healthcare seminars and meetings around the Waikato region. The findings of this study contribute to previous research that revealed over the last 20 years young parents have continued to report predominantly negative experiences in their maternity journey. Participants of this study reported experiences of unsolicited judgement and advice, a general lack of manaakitanga (care, empathy, respect), communication, and support from doctors, nurses, and midwives. The relatively small number of positive experiences shared in this study emphasises the importance of manaakitanga regardless of age. An unexpected finding was the impact that receptionists had on young parents’ healthcare experiences, as the face and entry point of healthcare services.

text: Te mana o te wahine: Young mothers healthcare experiences in pregnancy, birth, and into motherhood In Aotearoa-New Zealand being a young mother is often associated with clinical and societal ‘risks.’ Younger women have higher rates of maternal depression and suicide, complications during birth, and their babies are more likely to be born preterm, and of smaller gestational age and weight (Perinatal and Maternal Mortality Review Committee, 2012; Te Whatu Ora - Health New Zealand, 2023b, 2023a). Research also indicates that young mothers experience stigmatisation and discrimination that they attribute to their age and/or ethnicity (Adcock, 2016; Makowharemahihi et al., 2014; Rawiri, 2007; Ware, 2019).
In discussion with researchers, discrimination was the topic that young mothers at He Puaawai Teen Parent Centre wanted to talk about. They shared a strong desire to see change in the way that doctors, nurses, and midwives service young parents and were passionate about ensuring that future young mothers had more support. Thus, in responding to their call, 22 parents, including two fathers attending (or recent school-leavers of) He Puaawai Teen Parent Centre volunteered to participate in this study. This qualitative kaupapa Māori study employed a series of wānanga, individual kōrero, and an investigator-triangulation thematic analysis. The research questions explored both the positive and negative healthcare experiences of this cohort during pregnancy, birth, and into motherhood.
The aim of this study was to listen and learn about the experiences of these young parents and co-design informational and/or educational materials to help healthcare practitioners better understand and support young mothers/parents. To spread awareness of the experiences of these young parents, the co-design materials and findings of this study were disseminated via various healthcare seminars and meetings around the Waikato region. The findings of this study contribute to previous research that revealed over the last 20 years young parents have continued to report predominantly negative experiences in their maternity journey. Participants of this study reported experiences of unsolicited judgement and advice, a general lack of manaakitanga (care, empathy, respect), communication, and support from doctors, nurses, and midwives. The relatively small number of positive experiences shared in this study emphasises the importance of manaakitanga regardless of age. An unexpected finding was the impact that receptionists had on young parents’ healthcare experiences, as the face and entry point of healthcare services.

year: 2024