Stratigraphy and development of the Late Miocene-Early Pleistocene Hawke’s Bay forearc basin

A Late Miocene-Early Pleistocene mixed carbonate-siliciclastic sedimentary succession about 2 500 m thick in the Hawke’s Bay forearc basin is the focus of a basin analysis. The area under investigation covers 3 500 km2 of western and central Hawke’s Bay. The stratigraphy of Hawke’s Bay Basin is characterised by dramatic vertical and lateral facies changes and significant fluxes of siliciclastic sediment through the Late Miocene and Pliocene. This project aims to better understand the character and origin of the sedimentary succession in the basin. Geological mapping has been undertaken at a scale of 1:25000, with data managed in an ARCINFO geodatabase, following the database model employed in the IGNS QMap programme. Along the western margin of the basin there is progressive southward onlap of late Cenozoic strata on to basement. The oldest units are of Late Miocene (Tongaporutuan) age and the youngest onlap units are of latest Pliocene (Nukumaruan) age. Geological mapping of the basin fill places constraints on the magnitude (about 10 km) and timing (Pleistocene) of most of the offset on the North Island Shear Belt. Lithofacies have been described and interpreted representing fluvial, estuarine, shoreface and inner- to outer-shelf environments. Conglomerate facies are representative of sediment-saturated prograding fluvial braidplains and river deltas. These units are dominated by greywacke gravels and record the erosion of the Kaweka-Ahimanawa Ranges. Sandstone facies typically comprise very well sorted, clean non-cemented units of 10-50 m thickness that accumulated in innershelf environments. Siltstone facies probably accumulated in relatively quiet, middle- to outer-shelf water depths, and comprise well-sorted, firm non-cemented units with occasional tephra interbeds. Limestone facies represent examples of continent-attached cool-water carbonate systems that developed in response to strong tidal currents and a high nutrient flux during the Pliocene. These facies are examples of mixed siliciclastic-bioclastic sedimentary systems. Of these facies the widespread distribution and thickness of sandstone and limestone units present the most potential for hydrocarbon reservoirs. Similarly, the distribution of siltstone and mudstone beds provides adequate seal rocks. Mangapanian limestone facies have already been targeted as potential petroleum reservoirs (e.g. Kereru-1). Geological mapping suggests that potential hydrocarbon reservoir and seal rocks occur extensively in the subsurface

Systematic lithostratigraphy of the Neogene succession exposed in central parts of Hawke’s Bay Basin, eastern North Island, New Zealand

This report presents a systematic lithostratigraphy for the Neogene (Miocene–Recent) sedimentary succession in central parts of Hawke’s Bay Basin in eastern North Island, New Zealand. It has been built up chiefly from strata exposed in outcrop, but petroleum exploration drill hole data have also been incorporated to produce this stratigraphic synthesis. Most of the strata exposed in this part of the basin are of Late Miocene (Tongaporutuan, local New Zealand Stage) to Recent age, and the majority of this report focuses on these starta, with brief description of Middle and Early Miocene formations. A companion PR report (Kamp et al. 2007) contains stratigraphic columns for sections through the Neogene succession described in this report

Late Miocene – Early Pleistocene paleogeography of the onshore central Hawke’s Bay sector of the forearc basin, eastern North Island, New Zealand, and some implications for hydrocarbon prospectivity

The timing of trap formation in relation to the timing of source rock burial and maturation are important considerations in evaluating the hydrocarbon prospectivity of onshore parts of the forearc basin in central Hawke’s Bay. We describe here aspects of the Late Miocene to Early Pleistocene paleogeography for the area based on detailed field mapping and lithofacies analysis, to help constrain petroleum systems evaluations. Key conclusions are: • Most deformation of the forearc basin fill appears to be relatively young (i.e. post-2 Ma). This deformation has occurred after a major phase of Late Miocene to Pliocene sediment accumulation, and is particularly significant along the northwestern and southeastern margins of the basin. • The axis of the forearc basin in central Hawke’s Bay appears to have undergone little structural deformation. Gentle force and reverse faults in the subsurface may be suitable traps. • The most widespread potential reservoir beds are Miocene sandstone beds. • Potential hydrocarbon source rocks are mostly absent from western parts of the basin due to significant Neogene uplift and erosion. They are, however, probably still widely preserved beneath central parts of the basin where uplift and erosion have been much less pronounced. • Miocene structures within the axis of the basin, buried by the Late Miocene to Pleistocene siliciclastic succession, are likely exploration targets. The forearc basin has been substantially inverted along its western side since the latest Pliocene, resulting in erosion of older sediments, including potential source rocks, down to basement in ranges flanking its western side. The stratigraphy along the eastern margin of the forearc basin, and particularly the outcrop pattern of westward-younging Plio-Pleistocene limestones, records the development of faulting and folding associated with the elevation and growth of the inboard part of the accretionary wedge. Parts of the forearc basin succession have become involved in the accretionary wedge, which has migrated westward through time. Uplift of the inboard margin of the accretionary wedge since the latest Miocene helped to cause an interior seaway to develop to the west during the Pliocene. Distinctive coarse-grained bioclastic carbonate sediments of the Te Aute lithofacies were deposited along both margins of the seaway, which was most extensive during the Late Pliocene (Mangapanian). Although significant volumes of siliciclastic sediment were supplied to the basin during the Pliocene, strong tidal currents periodically swept much of these sediments northeastward. Tidal connections existed during the Pliocene into Wanganui Basin in the vicinity of Kuripapango and Manawatu Gorge. By the latest Pliocene (lower Nukumaruan), the interior seaway became closed in the south with uplift of the Mount Bruce block in northern Wairarapa. Potential reservoirs within the map area include both shelf and redeposited sandstone beds in the Miocene to Early Pliocene Tolaga Group. Thick, coarse-grained, variably cemented Plio-Pleistocene limestone lithofacies in the Mangaheia Group are widespread along the margins of the basin, and have been the targets for several past exploration programmes. However, drilling has shown that the attractiveness of the Pliocene limestone facies as reservoir beds is limited because they quickly pass laterally into siliciclastic mudstone away from the margins of the basin

The Benefits of Optimism in a Student-Instructor Relationship

The positive psychology movement of the past decade has produced an impressive amount of psychological literature devoted to studying the best of human attributes such as resilience, commitment, and optimism. This dramatic increase in available literature on optimism highlights a heightened awareness and interest in human proficiency, when so much of psychology has been traditionally devoted to the study of human deficiency. This research has lead to an increased understanding of what characteristics of an individual lead to facilitate various activities such as problem solving, leadership ability, income, achievement, sales, and job satisfaction. This study explored the relationship between positive affect and performance, specifically in reading, a skill used frequently in higher education. This study investigated if a comment from an instructor elicited a positive feeling in a student, and what impact that positive affect may have had upon a student\u27s reading performance

SB26-19/20: Resolution Regarding Sustainability Fee Referendum

SB26-19/20: Resolution Regarding Sustainability Fee Referendum Passed 17Y-3N-0A in the November 6,2019 ASUM Senate Meeting

SB61-19/20: Resolution Endorsing the Sustainability Fee Adjustment

SB61-19/20: Resolution Endorsing the Sustainability Fee Adjustment. This resolution passed on a 18Y-0N-1A vote during the March 25, 2020 meeting of the Associated Students of the University of Montana (ASUM)

SB29-19/20: Resolution Regarding Support for Migrating Sonocent\u27s Funding to IT Services

SB29-19/20: Resolution Regarding Support for Migrating Sonocent\u27s Funding to IT Services Passed 19Y-0N-1A in the November 6,2019 ASUM Senate Meetin

Virtual Reality: An Evidence-Based Guide for Occupational Therapy

Problem: Virtual reality (VR) is an emerging technology that serves to position the user in control of a virtual environment to maximize interest and function. VR is a context for intervention included in the Occupational Therapy Practice Framework: Domain and Process 3rd edition (OTPF-3; AOTA, 2014). It is crucial that occupational therapy (OT) practitioners enhance their knowledge about VR technology used by their clients to provide effective client-centered practice (AOTA, 2010). There is a lack of organization of the literature and research evidence regarding the use of VR as an intervention modality. While there has been a significant increase in recent literature supporting the use of VR in OT, there is a need for manuals and resources to guide clinicians in using VR as a therapeutic modality (Levac & Miller, 2013; Proffitt & Lange, 2015). Methods: An extensive literature review for articles regarding the use of the Xbox Kinect and Nintendo Wii within OT was conducted using five databases. Relevant data was extracted from each article related to the use of the Xbox Kinect or Nintendo Wii in intervention to synthesize the findings into charts. The construction of the charts followed the organization of the OTPF-3 (AOTA, 2014). Product: The authors of this product created an evidence-based resource to guide OT practitioners\u27 use of VR. The intended purpose of this product, Virtual Reality: An Evidence-Based Guide, is to assist OT practitioners\u27 adaptation and/or modification of VR activities to address individual client needs. Using this product as a guide to current knowledge and evidence regarding intervention in the context of VR, OT practitioners will be better equipped to make safe and effective choices. To further support development of literature regarding VR, the authors of this product recommended areas for future research

Use of steel and tantalum apparatus for molten Cd-Mg-Zn alloys

Steel and tantalum apparatus contains various ternary alloys of cadmium, zinc, and magnesium used in pyrochemical processes for the recovery of uranium-base reactor fuels. These materials exhibit good corrosion resistance at the high temperatures necessary for fuel separation in liquid metal-molten salt solvents