title: The Pacific infants performance scale: some preliminary and comparative New Zealand studies

authors: St George, Alison Margaret

abstract: The study and measurement of abilities in young children has been a field of early and continuing interest in psychology. Within this field it is possible to discern several major areas of inquiry. 
In attempting to draw up a schema of sorts it can be seen, first of all, that there have been many studies which broadly fall into the category of ' Developmental '. These studies have dealt with aspects of child development such as physical growth, motor development, perceptual development and so on (e.g. Birch & Lefford, 1967; Brozek, 1970; Gliner, Pick, Pick & Hales, 1969). 
Secondly, there have been what might be called 'Social Development ' studies, concerned with acquisition of various behaviours such as communication skills necessary for harmonious group behaviour, and the learning of appropriate roles (e.g. Baldwin, Baldwin, Hilton & Lambert, 1969; Selman, 1971). Many of these studies have been influenced by theories and investigations of ' personality development ' in children, particularly the ' child rearing ' studies (e.g. Ritchie & Ritchie, 1970; Sears, Maccoby & Levin, 1957; Whiting and Child, 1953). More recently there have been systematic observational studies of interaction patterns between children and significant others in their milieu.

text: The Pacific infants performance scale: some preliminary and comparative New Zealand studies The study and measurement of abilities in young children has been a field of early and continuing interest in psychology. Within this field it is possible to discern several major areas of inquiry. 
In attempting to draw up a schema of sorts it can be seen, first of all, that there have been many studies which broadly fall into the category of ' Developmental '. These studies have dealt with aspects of child development such as physical growth, motor development, perceptual development and so on (e.g. Birch & Lefford, 1967; Brozek, 1970; Gliner, Pick, Pick & Hales, 1969). 
Secondly, there have been what might be called 'Social Development ' studies, concerned with acquisition of various behaviours such as communication skills necessary for harmonious group behaviour, and the learning of appropriate roles (e.g. Baldwin, Baldwin, Hilton & Lambert, 1969; Selman, 1971). Many of these studies have been influenced by theories and investigations of ' personality development ' in children, particularly the ' child rearing ' studies (e.g. Ritchie & Ritchie, 1970; Sears, Maccoby & Levin, 1957; Whiting and Child, 1953). More recently there have been systematic observational studies of interaction patterns between children and significant others in their milieu.

year: 1972

title: Constraints on the evolution of Taranaki Fault from thermochronology and basin analysis: Implications for the Taranaki Fault play

authors: Kamp, Peter J.J.

subjects: Taranaki Basin

abstract: Taranaki Fault is the major structure defining the eastern margin of Taranaki Basin and marks the juxtaposition of basement with the Late Cretaceous-Paleogene succession in the basin. Although the timing of the basement over-thrusting on Taranaki Fault and subsequent marine onlap on to the basement block are well constrained as having occurred during the Early Miocene, the age of formation of this major structure, its character, displacement history and associated regional vertical movement during the Late Cretaceous- Recent are otherwise poorly known. Here we have applied (i) apatite fission track thermochronology to Mesozoic basement encountered in exploration holes and in outcrop to constrain the amount and timing of Late Cretaceous-Eocene exhumation of the eastern side of the fault, (ii) basin analysis of the Oligocene and Miocene succession east of the fault to establish the late-Early Miocene - Early Pliocene subsidence history, and (iii), regional porosity-bulk density trends in Neogene mudstone to establish the late uplift and tilting of eastern Taranaki Basin margin, which may have been associated with the main period of charge of the underlying Taranaki Fault play.
We make the following conclusions that may be useful in assessing the viability of the Taranaki Fault play. (1) Mid-Cretaceous Taniwha Formation, intersected in Te Ranga-1 was formerly extensive across the western half of the Kawhia Syncline between Port Waikato and Awakino. (2) Taranaki Fault first formed as a normalfault during the Late Cretaceous around 85±10 Ma, and formed the eastern boundary of the Taranaki Rift-Transform basin. (3) Manganui Fault, located onshore north of Awakino, formed as a steeply east dipping reverse fault and accommodated about four km of displacement during the mid-Cretaceous. (4) Uplift and erosion, involving inversion of Early Oligocene deposits, occurred along the Herangi High during the Late Oligocene. This may have been associated with initial reverse movement on Taranaki Fault. (5) During the Early Miocene (Otaian Stage) the Taranaki and Manganui Faults accommodated the westward transport of Murihiku basement into the eastern margin of Taranaki Basin, but the amount of topography generated over the Herangi High can only have been a few hundred metres in elevation. (6) The Altonian (19-16 Ma) marked the start of the collapse of the eastern margin of Taranaki Basin that lead during the Middle Miocene to the eastward retrogradation of the continental margin wedge into the King Country region. During the Late Miocene, from about 11 Ma, a thick shelf-slope continental margin wedge prograded northward into the King Country region and infilled it (Mt Messenger, Urenui, Kiore and Matemateaonga Formations). (7) During the Pliocene and Pleistocene the whole of central New Zealand, including the eastern margin of Taranaki Basin, became involved in long wavelength up-doming with 1-2 km erosion of much of the Neogene succession in the King Country region. This regionally elevated the Taranaki Fault play into which hydrocarbons may have migrated from the Northern Graben region.

text: Constraints on the evolution of Taranaki Fault from thermochronology and basin analysis: Implications for the Taranaki Fault play Taranaki Fault is the major structure defining the eastern margin of Taranaki Basin and marks the juxtaposition of basement with the Late Cretaceous-Paleogene succession in the basin. Although the timing of the basement over-thrusting on Taranaki Fault and subsequent marine onlap on to the basement block are well constrained as having occurred during the Early Miocene, the age of formation of this major structure, its character, displacement history and associated regional vertical movement during the Late Cretaceous- Recent are otherwise poorly known. Here we have applied (i) apatite fission track thermochronology to Mesozoic basement encountered in exploration holes and in outcrop to constrain the amount and timing of Late Cretaceous-Eocene exhumation of the eastern side of the fault, (ii) basin analysis of the Oligocene and Miocene succession east of the fault to establish the late-Early Miocene - Early Pliocene subsidence history, and (iii), regional porosity-bulk density trends in Neogene mudstone to establish the late uplift and tilting of eastern Taranaki Basin margin, which may have been associated with the main period of charge of the underlying Taranaki Fault play.
We make the following conclusions that may be useful in assessing the viability of the Taranaki Fault play. (1) Mid-Cretaceous Taniwha Formation, intersected in Te Ranga-1 was formerly extensive across the western half of the Kawhia Syncline between Port Waikato and Awakino. (2) Taranaki Fault first formed as a normalfault during the Late Cretaceous around 85±10 Ma, and formed the eastern boundary of the Taranaki Rift-Transform basin. (3) Manganui Fault, located onshore north of Awakino, formed as a steeply east dipping reverse fault and accommodated about four km of displacement during the mid-Cretaceous. (4) Uplift and erosion, involving inversion of Early Oligocene deposits, occurred along the Herangi High during the Late Oligocene. This may have been associated with initial reverse movement on Taranaki Fault. (5) During the Early Miocene (Otaian Stage) the Taranaki and Manganui Faults accommodated the westward transport of Murihiku basement into the eastern margin of Taranaki Basin, but the amount of topography generated over the Herangi High can only have been a few hundred metres in elevation. (6) The Altonian (19-16 Ma) marked the start of the collapse of the eastern margin of Taranaki Basin that lead during the Middle Miocene to the eastward retrogradation of the continental margin wedge into the King Country region. During the Late Miocene, from about 11 Ma, a thick shelf-slope continental margin wedge prograded northward into the King Country region and infilled it (Mt Messenger, Urenui, Kiore and Matemateaonga Formations). (7) During the Pliocene and Pleistocene the whole of central New Zealand, including the eastern margin of Taranaki Basin, became involved in long wavelength up-doming with 1-2 km erosion of much of the Neogene succession in the King Country region. This regionally elevated the Taranaki Fault play into which hydrocarbons may have migrated from the Northern Graben region.

year: 2004

title: Rangatahi of Ngāi Te Rangi Iwi: Cultural belonging and connectedness

authors: Benton, Chelsea

subjects: Māori

abstract: Rangatahi Māori (Māori youth) have one of the highest suicide rates in the OECD, they leave school earlier and with less qualifications, and suffer from higher rates of unemployment, hospitalisation and conduct and substance disorders and abuse than non-Māori. Sadly, many rangatahi move into adulthood only to experience poorer physical and mental health, shorter lifespans, and lower socioeconomic status compared to that of non-Māori. With these poor health outcomes for rangatahi Māori in mind this research explores the nature of Māori identities as a foundation for wellness, meaning, and flourishing. More importantly, this research takes into consideration the negative impacts of the colonisation of Māori and their cultural identity and the inter-generational effects of this long term systematic nature of disadvantage. I posit that cultural connectedness and belonging can foster healthy psychological and behavioural outcomes for rangatahi Māori. The mixed-method approach taken within this research sits within a Kaupapa Māori framework and draws upon accounts of 16 rangatahi Māori, aged between 10 and 14 years, who participated in a Ngāi Te Rangi Iwi based leadership development programme that reconnects rangatahi Māori with traditional customs and practices of their ancestors to enhance their health and wellbeing. Findings suggest that connectedness and belonging are manifest through practices such as Pēpeha, whakapapa, and Whakataukī/whakatauāki and rangatahi Māori draw on this cultural knowledge base and cultural practices to empower themselves, their whānau, hapū and Iwi. Rangatahi Māori in this sample also identified that whānau was most important in their lives followed by engagement in Māori culture. Findings highlight how Iwi organisations are stepping up to lead their people to a brighter future. For Māori, engaging with their Māoritanga and Te Ao Māori not only addresses the negative impacts of colonialism, but unlocks cultural potential, and an enhanced sense of self which serves to empower rangatahi Māori, their whānau, hapū and Iwi.

text: Rangatahi of Ngāi Te Rangi Iwi: Cultural belonging and connectedness Rangatahi Māori (Māori youth) have one of the highest suicide rates in the OECD, they leave school earlier and with less qualifications, and suffer from higher rates of unemployment, hospitalisation and conduct and substance disorders and abuse than non-Māori. Sadly, many rangatahi move into adulthood only to experience poorer physical and mental health, shorter lifespans, and lower socioeconomic status compared to that of non-Māori. With these poor health outcomes for rangatahi Māori in mind this research explores the nature of Māori identities as a foundation for wellness, meaning, and flourishing. More importantly, this research takes into consideration the negative impacts of the colonisation of Māori and their cultural identity and the inter-generational effects of this long term systematic nature of disadvantage. I posit that cultural connectedness and belonging can foster healthy psychological and behavioural outcomes for rangatahi Māori. The mixed-method approach taken within this research sits within a Kaupapa Māori framework and draws upon accounts of 16 rangatahi Māori, aged between 10 and 14 years, who participated in a Ngāi Te Rangi Iwi based leadership development programme that reconnects rangatahi Māori with traditional customs and practices of their ancestors to enhance their health and wellbeing. Findings suggest that connectedness and belonging are manifest through practices such as Pēpeha, whakapapa, and Whakataukī/whakatauāki and rangatahi Māori draw on this cultural knowledge base and cultural practices to empower themselves, their whānau, hapū and Iwi. Rangatahi Māori in this sample also identified that whānau was most important in their lives followed by engagement in Māori culture. Findings highlight how Iwi organisations are stepping up to lead their people to a brighter future. For Māori, engaging with their Māoritanga and Te Ao Māori not only addresses the negative impacts of colonialism, but unlocks cultural potential, and an enhanced sense of self which serves to empower rangatahi Māori, their whānau, hapū and Iwi.

year: 2019