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1

Sagala, Iko, and Mark Tingay. "Analysis of overpressure and its generating mechanisms in the northern Carnarvon Basin from drilling data." APPEA Journal 52, no. 1 (2012): 375. http://dx.doi.org/10.1071/aj11030.

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The Northern Carnarvon Basin is one of Australia’s most prolific hydrocarbon basins. Overpressure has been encountered in numerous wells drilled in the Northern Carnarvon Basin. Knowledge of overpressure distribution is important for drilling and exploration strategies, and understanding the origin of overpressure is essential for applying reliable pore pressure prediction techniques. Unconventional pore pressure indicators—primarily drilling kicks and the presence of connection gas—were used to improve an updated distribution of overpressure and to investigate the origin of overpressure in th
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Ladbrook, Megan, Eddie J. B. van Etten, and William D. Stock. "Contemporary Fire Regimes of the Arid Carnarvon Basin Region of Western Australia." Fire 1, no. 3 (December 14, 2018): 51. http://dx.doi.org/10.3390/fire1030051.

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This study investigates the fire regime for the arid Carnarvon Basin region of Western Australia using remotely sensed imagery. A fire history database was constructed from satellite images to characterise the general fire regime and determine any effect of vegetation types and pre-fire weather and climate. The study area was divided into two sections (northern and southern) due to their inherently different vegetation and climate. A total of 23.8% (15,646 km2) of the study area was burnt during the 39-year study period. Heathland vegetation (54%) burnt the most extensively in the southern stu
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Baillie, P. W., and E. Jacobson. "STRUCTURAL EVOLUTION OF THE CARNARVON TERRACE, WESTERN AUSTRALIA." APPEA Journal 35, no. 1 (1995): 321. http://dx.doi.org/10.1071/aj94020.

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The under-explored Carnarvon Terrace is situated offshore of the Cape Range area in the Carnarvon Basin near the boundary of the Gascoyne and Exmouth Sub-basins. The stratigraphy of the area is controlled by only two wells (Pendock-1, Yardie East-1), but several onshore wells aid interpretation of seismic data.Understanding of the structural evolution of the region is facilitated by interpretation of a high-resolution non-exclusive seismic survey acquired by Geco-Prakla in 1993 (GPCTR-93 Survey).Three major tectonic stages are responsible for the structural configuration of the region:Late Pal
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Przeslawski, Rachel, Matthew A. McArthur, and Tara J. Anderson. "Infaunal biodiversity patterns from Carnarvon Shelf (Ningaloo Reef), Western Australia." Marine and Freshwater Research 64, no. 6 (2013): 573. http://dx.doi.org/10.1071/mf12240.

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Infauna are important in many ecological processes but have been rarely considered in biodiversity assessments of coral reefs and surrounding areas. We surveyed infaunal assemblages and associated environmental factors (depth, seabed reflectance, sediment characteristics) in three areas (Mandu, Point Cloates, Gnaraloo) along the Carnarvon Shelf, Western Australia. This region supports Ningaloo Reef, a relatively pristine coral reef protected by the Ningaloo Marine Park and a Commonwealth marine reserve. Macrofauna were sampled with a Smith-McIntyre grab and sieved through 500 µm. A total of 42
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Gorter, J. D., and J. M. Davies. "UPPER PERMIAN CARBONATE RESERVOIRS OF THE NORTH WEST SHELF AND NORTHERN PERTH BASIN, AUSTRALIA." APPEA Journal 39, no. 1 (1999): 343. http://dx.doi.org/10.1071/aj98019.

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The Perth, Carnarvon, Browse, and Bonaparte basins contain Permian shallowmarine carbonates. Interbedded with clastic oil and gas reservoirs in the northern Perth Basin (Wagina Formation), and gas reservoirs in the Bonaparte Basin (Cape Hay and Tern formations), these carbonates also have the potential to contain significant hydrocarbon reservoirs. Limestone porosity may be related to the primary depositional fabric, or secondary processes such as dolomitisation, karstification, and fracturing. However, in the Upper Permian interval of the North West Shelf and northern Perth Basin, where there
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6

Cooper, Martin, Richard Midford, and Julie Anne Jaegar. "Carnarvon Partysafe: Designing a Community Mobilisation Project in Western Australia's Remote North West." Australian Journal of Primary Health 7, no. 3 (2001): 63. http://dx.doi.org/10.1071/py01048.

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Recent studies are increasingly shifting away from viewing drug and alcohol problems as individual medical disorders and recognising the significant role of environmental and community factors. In keeping with this, the Partysafe project, being implemented in the remote North West town of Carnarvon in Western Australia (WA), is utilising a community mobilisation approach to reducing harm associated with alcohol consumption in private residences. Carnarvon, like most rural communities in WA, has a higher rate of alcohol consumption than in the metropolitan region, hence its selection as the tar
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CATULLO, RENEE A., PAUL DOUGHTY, J. DALE ROBERTS, and J. SCOTT KEOGH. "Multi-locus phylogeny and taxonomic revision of Uperoleia toadlets (Anura: Myobatrachidae) from the western arid zone of Australia, with a description of a new species." Zootaxa 2902, no. 1 (June 1, 2011): 1. http://dx.doi.org/10.11646/zootaxa.2902.1.1.

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We generated a multi-locus phylogeny to test monophyly and distributional limits in Australian toadlets of the genus Uperoleia from the western arid zone of Australia. The molecular data were used in combination with a detailed assessment of morphological variation and some data on call structure to complete a taxonomic revision of the species that occur in this region. Our work reveals the existence of not two but five species in the region. Uperoleia russelli is restricted to the Carnarvon and Gascoyne Regions south of the Pilbara. Uperoleia micromeles is distributed from the Tanami Desert t
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8

Tingate, P. R., A. Khaksar, P. van Ruth, D. Dewhurst, M. Raven, H. Young, R. Hillis, and K. Dodds. "GEOLOGICAL CONTROLS ON OVERPRESSURE IN THE NORTHERN CARNARVON BASIN." APPEA Journal 41, no. 1 (2001): 573. http://dx.doi.org/10.1071/aj00029.

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A small, but significant fraction of wells drilled in the Northern Carnarvon Basin have encountered problems with overpressure: better pore pressure prediction would improve safety and economy for drilling operations. In the Northern Carnarvon Basin the occurrence of overpressure and likely mechanisms are under investigation as part of the Australian Petroleum Cooperative Research Centre (APCRC) Research Program on Pore Pressure Prediction. Previous workers have proposed a number of mechanisms as the main cause of overpressure including undercompaction, hydrocarbon generation, horizontal stres
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9

Blevin, J. E. "EXPLORATION HIGHLIGHTS FOR 2006." APPEA Journal 47, no. 2 (2007): 631. http://dx.doi.org/10.1071/aj06056.

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Key business indicators show an upward trend in exploration activity in Australia during 2006. The year was marked by fluctuating high oil prices, a strong uptake of acreage in most basins, and increased levels of drilling activity and seismic acquisition. Market demand for product, production infrastructure and the fruition of several development projects have pushed the level of exploration activity in both offshore and onshore basins. Despite this trend and the spread of tenements, almost all petroleum discoveries made during 2006 were located within 15 km of existing (but often undeveloped
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10

Cockbain, A. E. "THE NORTH WEST SHELF." APPEA Journal 29, no. 1 (1989): 529. http://dx.doi.org/10.1071/aj88040.

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The region of the North West Shelf dealt with in this paper is underlain by three of the four basins which make up the Westralian Superbasin. The Bonaparte Basin lies outside the scope of this paper; the other basins are the Browse Basin, the offshore Canning Basin, here named the Western Canning Basin, and the offshore Carnarvon Basin, here called the Northern Carnarvon Basin. Sediments belonging to ten depositional sequences (Pz5, Mzl to Mz5, and Czl to Cz4) are present in the basins, the oldest being of Late Carboniferous and Permian age (Pz5).Deposition commenced in rift (interior fracture
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11

Cowley, R., and G. W. O'Brien. "IDENTIFICATION AND INTERPRETATION OF LEAKING HYDROCARBONS USING SEISMIC DATA:A COMPARATIVE MONTAGE OF EXAMPLES FROM THE MAJOR FIELDS IN AUSTRALIA'S NORTHWEST SHELF AND GIPPSLAND BASIN." APPEA Journal 40, no. 1 (2000): 119. http://dx.doi.org/10.1071/aj99008.

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An extensive volume of 3D seismic data over a number of oil and gas fields in Australia's North West Shelf and Gippsland Basin has been examined for evidence of the effects of hydrocarbon migration and/or leakage. For comparative purposes, 2D and 3D data have also been studied over a number of adjacent traps, including dry traps and partially to completely breached accumulations. Fields and traps investigated include Bayu-Undan, Jabiru, Skua, Swift and Tahbilk in the Bonaparte Basin, Cornea in the Browse Basin, North Rankin, Chinook, Macedon, Enfield and Zeewulf in the Carnarvon Basin, and Kin
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12

Bailey, Adam H. E., Rosalind C. King, Simon P. Holford, and Martin Hand. "Extending interpretations of natural fractures from the wellbore using 3D attributes: The Carnarvon Basin, Australia." Interpretation 4, no. 1 (February 1, 2016): SB107—SB129. http://dx.doi.org/10.1190/int-2015-0113.1.

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Natural fractures can be identified in wellbores using electric resistivity image logs; however, the challenge of predicting fracture orientations, densities, and probable contribution to subsurface fluid flow away from the wellbore remains. Regional interpretations of fracture sets are generally confined to areas featuring an extensive reservoir analog outcrop. We have made use of extensive data sets available in Western Australia’s Northern Carnarvon Basin to map subsurface natural fractures, contributing to a regional understanding of fracture sets that can be applied to broader parts of th
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13

Beaton, J. M. "Excavations at Rainbow Cave and Wanderer's Cave: two rockshelters in the Carnarvon Range, Queensland." Queensland Archaeological Research 8 (January 1, 1991): 3–32. http://dx.doi.org/10.25120/qar.8.1991.117.

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If the state of Queensland can be said to have true "uplands", then they are to be found in the southern and central region of the state in that place Archibald Meston (1895) called the "Home of the Rivers". There, some 400km inland from Australia's eastern coast and some 600km south of the Tropic of Capricorn, the uplifted and heavily weathered Triassic sandstones form a conspicuous link in the north-south trending mountains collectively referred to as "The Great Dividing Range". These ancient sandstones seldom rise above 650m elevation, and never more than the prominence of Black Alley Peak
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14

O’Brien, G. W., R. Cowley, G. Lawrence, A. K. Williams, M. Webster, P. Tingate, and S. Burns. "MIGRATION, LEAKAGE AND SEEPAGE CHARACTERISTICS OF THE OFFSHORE CANNING BASIN AND NORTHERN CARNARVON BASIN: IMPLICATIONS FOR HYDROCARBON PROSPECTIVITY." APPEA Journal 43, no. 2 (2003): 149. http://dx.doi.org/10.1071/aj02072.

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RadarSat and ERS Synthetic Aperture Radar (SAR) satellite data have been used for oil slick mapping as part of a systematic interpretative study of the offshore Canning Basin, as well as part of the northern Carnarvon Basin, extending from the inner shelf to the abyssal plain. These seepage data have been integrated with regional geological data, more than 12,000 km of reprocessed Airborne Laser Fluorosensor (ALF) survey data, seismic DHI indicators, water column geochemical sniffer data, potential field data, earthquake data and 2D Petromod basin modelling, to provide new insights into the re
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15

Borissova, Irina, and Gabriel Nelson. "Petroleum potential of the offshore southern Carnarvon Basin—insights from new Geoscience Australia data." APPEA Journal 51, no. 2 (2011): 746. http://dx.doi.org/10.1071/aj10126.

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In 2008–9, under the Offshore Energy Security Program, Geoscience Australia (GA) acquired 650 km of seismic data, more than 3,000 km of gravity and magnetic data, and, dredge samples in the southern Carnarvon Basin. This area comprises the Paleozoic Bernier Platform and southern part of the Mesozoic Exmouth Sub-basin. The new seismic and potential field data provide a new insight into the structure and sediment thickness of the deepwater southernmost part of the Exmouth Sub-basin. Mesozoic depocentres correspond to a linear gravity low, in water depths between 1,000–2,000 m and contain between
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16

Blevin, J. E., A. E. Stephenson, and B. G. West. "THE STRUCTURAL AND STRATIGRAPHIC FRAMEWORK OF THE BEAGLE SUB-BASIN, IMPLICATIONS FOR HYDROCARBON MIGRATION AND TRAP DEVELOPMENT." APPEA Journal 33, no. 1 (1993): 105. http://dx.doi.org/10.1071/aj92009.

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The Beagle Sub-basin is situated in the northernmost Carnarvon Basin, northeast of Dampier, West Australia. Twenty years of exploration in the sub-basin has yielded disappointing results, and despite the drilling of ten wells, the area is considered an under-explored region of the Northern Carnarvon Basin. A regional study of open-file geophysical and geological data from the Beagle Sub-basin was undertaken in anticipation of gazettal of the area in late 1992.Regional mapping of structural elements in the basin included:a complex, E/W to NE/SW-trending basin margin fault system;N/S-trending in
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17

Smith, S. A., P. R. Tingate, C. M. Griffths, and J. N. F. Hull. "THE STRUCTURAL DEVELOPMENT AND PETROLEUM POTENTIAL OF THE ROEBUCK BASIN." APPEA Journal 39, no. 1 (1999): 364. http://dx.doi.org/10.1071/aj98020.

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The Roebuck Basin is a sparsely explored, frontier province located between the Carnarvon and Browse basins on Australia's North West Shelf. Mapping of the main structural and depositional elements of the basin has led to the identification of new features and elucidated the basin's tectonic history.The newly-identified Oobagooma High is a 25 km wide north-south oriented, elongate structure that separates the Oobagooma and Rowley sub-basins at the Palaeozoic level. This structure links with the Bedout High to form a major hinge zone that stretches across the entire basin.In the study area, thr
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18

Pryer, L. L., K. K. Romine, T. S. Loutit, and R. G. Barnes. "CARNARVON BASIN ARCHITECTURE AND STRUCTURE DEFINED BY THE INTEGRATION OF MINERAL AND PETROLEUM EXPLORATION TOOLS AND TECHNIQUES." APPEA Journal 42, no. 1 (2002): 287. http://dx.doi.org/10.1071/aj01016.

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The Barrow and Dampier Sub-basins of the Northern Carnarvon Basin developed by repeated reactivation of long-lived basement structures during Palaeozoic and Mesozoic tectonism. Inherited basement fabric specific to the terranes and mobile belts in the region comprise northwest, northeast, and north–south-trending Archaean and Proterozoic structures. Reactivation of these structures controlled the shape of the sub-basin depocentres and basement topography, and determined the orientation and style of structures in the sediments.The Lewis Trough is localised over a reactivated NEtrending former s
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19

Huang, Zhi, Matthew McArthur, Rachel Przeslawski, Justy Siwabessy, Scott Nichol, and Brendan Brooke. "Predictive mapping of soft-bottom benthic biodiversity using a surrogacy approach." Marine and Freshwater Research 65, no. 5 (2014): 409. http://dx.doi.org/10.1071/mf13104.

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A key requirement for informed marine-zone management is an understanding of the spatial patterns of marine biodiversity, often measured as species richness, total abundance or presence of key taxa. In the present study, we focussed on the diversity of benthic infauna and applied a predictive modelling approach to map biodiversity patterns for three study sites on the tropical Carnarvon shelf of Western Australia. A random forest decision tree model was used to generate spatial predictions of two measures of infaunal diversity, namely, species richness and total abundance. Results explained be
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20

Wallace, M. W., E. Condilis, A. Powell, J. Redfearn, K. Auld, M. Wiltshire, G. Holdgate, and S. Gallagher. "GEOLOGICAL CONTROLS ON SONIC VELOCITY IN THE CENOZOIC CARBONATES OF THE NORTHERN CARNARVON BASIN, NORTH WEST SHELF, WESTERN AUSTRALIA." APPEA Journal 43, no. 1 (2003): 385. http://dx.doi.org/10.1071/aj02020.

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The Cenozoic carbonates of the Bounty-Talisman region can be divided into five major facies. From oldest to youngest, these are: Paleocene to Eocene basinal facies, Oligocene to Miocene slope-canyon facies, Oligocene to Miocene shelf facies, Oligocene to Miocene near-shore facies, and Pliocene-Quaternary shelf facies. This represents a shallowing-upwards cycle up to the late Miocene, followed by a significant transgression and a return to more open marine conditions in the Pliocene- Quaternary. The dominant geological processes controlling sonic velocity in the Cenozoic carbonates are physical
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21

Bekele, E. B., M. D. Johnson, and W. G. Higgs. "NUMERICAL MODELLING OF OVERPRESSURE GENERATION IN THE BARROW SUB-BASIN, NORTHWEST AUSTRALIA." APPEA Journal 41, no. 1 (2001): 595. http://dx.doi.org/10.1071/aj00030.

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A numerical basin modelling approach was used to investigate the hydrodynamics and development of overpressures in a Jurassic Prospect in the Greater Gorgon area of the Barrow Sub-basin. Abnormally large fluid pressures have been encountered by numerous exploratory wells in the Carnarvon Basin; however, the mechanisms responsible for overpressuring were uncertain. To better evaluate the risk of encountering overpressures while drilling Jurassic targets in the area, quantitative basin modelling was conducted. Groundwater flow, heat transfer, and hydrocarbon generation were simulated along two g
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22

HARRISON, SOPHIE E., MICHAEL G. RIX, MARK S. HARVEY, and ANDREW D. AUSTIN. "Systematics of the Australian spiny trapdoor spiders of the genus Blakistonia Hogg (Araneae: Idiopidae)." Zootaxa 4518, no. 1 (November 12, 2018): 1. http://dx.doi.org/10.11646/zootaxa.4518.1.1.

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A combined molecular and morphological approach was used to revise the Australian spiny trapdoor spiders of the genus Blakistonia Hogg. Where possible, our molecular approach used sequence data from the COI barcoding gene, which were analysed using Bayesian, RAxML and neighbour-joining approaches. These molecular data were combined with morphology to describe and diagnose the genus, to redescribe the type (and only previously valid) species, B. aurea Hogg, 1902, and to diagnose, describe and map 19 new species: B. bassi sp. n., B. bella sp. n., B. birksi sp. n., B. carnarvon sp. n., B. emmotti
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Beacher, G. J. "PRESSURE STUDY OF THE FLACOURT FORMATION AQUIFER IN THE THEVENARD ISLAND AREA OF THE BARROW SUB-BASIN." APPEA Journal 38, no. 1 (1998): 438. http://dx.doi.org/10.1071/aj97021.

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Thevenard Island area lies in the offshore Carnarvon Basin off the northwest coast of Western Australia. The Flacourt Formation of the Cretaceous Barrow Group sequence is the primary oil-producing reservoir. West Australian Petroleum Pty Limited (WAPET) as operator on behalf of its participants (Chevron, Texaco, Shell and Mobil) has been producing from this reservoir since 1989. It has widely been held that in this area the relatively thick, multi-darcy Barrow Group oil accumulations have had infinite aquifer pressure support with no regional draw-down effect.After the commencement of oil prod
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Hunter, P. C. "PREPARATION AND IMPLEMENTATION OF A SAFETY MANAGEMENT SYSTEM IN BHPP." APPEA Journal 37, no. 1 (1997): 657. http://dx.doi.org/10.1071/aj96046.

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BHP is a leading global resources company which comprises four main business groups: BHP Copper, BHP Minerals, BHP Steel and BHP Petroleum. BHP Petroleum (BHPP) global operations are divided into four Regions and Australia/Asia Region is responsible for exploration, production, field development and joint ventures in the Asia-Pacific region. In Australia, the Company's largest producing assets are its shares of the Gippsland oil and gas fields in Bass Strait and the North West Shelf project in Western Australia.BHPP operates three Floating Production, Storage and Offloading (FPSO) vessels-Jabi
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Paten, Tom. "The prospectivity of the Late Triassic intervals in the outboard Exmouth Plateau, Western Australia." APPEA Journal 60, no. 2 (2020): 742. http://dx.doi.org/10.1071/aj19173.

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The Exmouth Plateau is a deep-water plateau on the Australian continental margin underlain by 10–15 km of flat-lying, tilted and block-faulted Paleozoic–Mesozoic sedimentary rocks, which were deposited predominantly during periods of extension before continental break-up commenced in the middle Jurassic. The recent acquisition of the Mawson MC3D broadband seismic survey provides a modern, high-quality dataset located ~230 km to the north-west of Dampier, in the outboard Exmouth Plateau, in a relatively under-explored portion of the Northern Carnarvon Basin. The Late Triassic Mungaroo Formation
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Stejskal, I. V. "EXPLORATION IN SENSITIVE AREAS: CONVINCING THE COMMUNITY." APPEA Journal 35, no. 1 (1995): 822. http://dx.doi.org/10.1071/aj94059.

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Hadson Carnarvon Pty Ltd (Hadson), on behalf of the Joint Venture Partners, operates permits EP342 and TP/9 located at the northern end of Exmouth gulf, to the east of Cape Range peninsula, Western Australia. The Exmouth region is known for the Ningaloo Reef, and for its diving and recreational fishing. The area also supports a large commercial prawn fishery. Many marine areas in the Exmouth region are regarded as being environmentally sensitive with several areas of conservation value.The partners were committed to drilling two wells in EP342 and TP/9 in 1993 as part of the obligations under
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Lockhart, D., and D. Spring. "PESA Australian exploration review 2018." APPEA Journal 59, no. 2 (2019): 493. http://dx.doi.org/10.1071/aj18284.

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Available data for 2018 indicates that exploration activity is on the rise in Australia, compared to 2017, and this represents a second year of growth in exploration activity in Australia. There has been an increase in area under licence by 92 000 km2, reversing the downward trend in area under licence that commenced in 2014. Since 2016, exploratory drilling within Australia has seen a continued upward trend in both the number of wells drilled and the percentage of total worldwide. Onshore, 77 conventional exploration and appraisal wells were spudded during the year. Offshore, exploration and
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Wakelin-King, Gordon. "Highlights and trends in exploration 2009." APPEA Journal 50, no. 1 (2010): 113. http://dx.doi.org/10.1071/aj09008.

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2009 saw an overall decrease from high activity from 2008, levelling off in the December quarter as the economy stabilised. Unsurprisingly, most activity was in offshore Western Australia and on coal seam methane (CSM) in Queensland. Highlights include: good results in the Carnarvon and Browse basins for Western Australian operators, interest in Karoon and Conoco-Phillips’ enigmatic Poseidon project, over 180 CSM exploration wells in Queenslandd, and a relatively busy year for Tasmania. Western Australian seismic acquisition approached 10,000 km of 2D and 25,000 km2 of 3D for 38* wells and suc
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Mory, A. J., and R. P. lasky. "INTEGRATING SEISMIC, GRAVITY AND AEROMAGNETIC DATA IN THE STRUCTURAL INTERPRETATION OF THE MERLINLEIGH SUB-BASIN, WESTERN AUSTRALIA." APPEA Journal 37, no. 1 (1997): 205. http://dx.doi.org/10.1071/aj96012.

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The southern Merlinleigh Sub-basin is a frontier area for petroleum exploration within the onshore Southern Carnarvon Basin, with limited seismic coverage and only two deep exploration wells. High resolution aeromag- netic and semi-detailed gravity data acquired in 1995 provide relatively low cost structural inf ormation"comple- mentary to the regional seismic coverage.Two-dimensional seismic data can be mapped with confidence if the lines are closely spaced. By identifying lineaments on potential-field images, orientations for structures within the sedimentary succession, and at basement or i
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Ryan, Georgina, George Bernardel, John Kennard, Andrew T. Jones, Graham Logan, and Nadege Rollet. "A pre-cursor extensive Miocene reef system to the Rowley Shoals reefs, Western Australia: evidence for structural control of reef growth or natural hydrocarbon seepage?" APPEA Journal 49, no. 1 (2009): 337. http://dx.doi.org/10.1071/aj08021.

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Numerous Miocene reefs and related carbonate build-ups have been identified in the Rowley Shoals region of the central North West Shelf, offshore Western Australia. The reefs form part of an extensive Miocene reef tract over 1,600 km long, which extended northward into the Browse and Bonaparte basins and southward to North West Cape in the Carnarvon Basin—comparable in length to the modern Great Barrier Reef. Growth of the vast majority of these Miocene reefs failed to keep pace with relative sea-level changes in the latest Miocene, whereas reef growth continued on the central North West Shelf
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Bernecker, Tom. "The 2010 Australian offshore release for petroleum exploration." APPEA Journal 50, no. 1 (2010): 5. http://dx.doi.org/10.1071/aj09002.

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The Australian Government formally releases new offshore exploration areas at the annual APPEA conference. In 2010, thirty-one areas in five offshore basins are being released for work program bidding. Closing dates for bid submissions are either six or twelve months after the release date—i.e. 11 November 2010 and 12 May 2011—depending on the exploration status in these areas and on data availability. The 2010 release areas are located in Commonwealth waters offshore Northern Territory, Western Australia and South Australia, comprising intensively explored areas close to existing production a
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32

Siverson, Mikael. "A new large lamniform shark from the uppermost Gearle Siltstone (Cenomanian, Late Cretaceous) of Western Australia." Transactions of the Royal Society of Edinburgh: Earth Sciences 90, no. 1 (1999): 49–66. http://dx.doi.org/10.1017/s0263593300002509.

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AbstractAn association of 100 teeth and 15 vertebrae from a large, lamniform shark, is described from the uppermost part of the Gearle Siltstone in the Giralia Anticline, Southern Carnarvon Basin, Western Australia. The material represents a new genus and species: Cardabiodon ricki. The taxon is referred to the new family Cardabiodontidae on the basis of its dental formula and uniquely oversized lower lateroposterior teeth. Other characteristic features include a strong dignathic heterodonty and the presence of four anterior and approximately 14 lateroposterior toothfiles in both the upper and
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33

Percival, I. G., and P. M. Cooney. "PETROLEUM GEOLOGY OF THE MERLINLEIGH SUB-BASIN, WESTERN AUSTRALIA." APPEA Journal 25, no. 1 (1985): 190. http://dx.doi.org/10.1071/aj84017.

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Esso's recent drilling program in the Merlinleigh Sub-basin, onshore Carnarvon Basin, represents the culmination of the first phase of concerted exploration activity in the area since the WAPET era of the 1960s. The region is unusual among Australian petroleum provinces in having excellent exposures of reservoir, source and seal rocks of Palaeozoic age. While both Esso wells (Burna 1 and Gascoyne 1) failed to encounter hydrocarbons in the primary Wooramel Group play, encouraging potential still exists. The reservoir in the Wooramel Group play is the Early Permian Moogooloo Sandstone, a fluviod
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34

Bernecker, Thomas. "Geological overview of the 2011 offshore acreage release for petroleum exploration." APPEA Journal 51, no. 1 (2011): 7. http://dx.doi.org/10.1071/aj10002.

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The Australian Government formally releases new offshore exploration areas at the annual APPEA conference. In 2011, 29 areas in eight offshore basins are being released for work program bidding. Closing dates for bid submissions are either six or 12 months after the release date (i.e. 13 October 2011 and 12 April 2012)–this depends on the exploration status in these areas and on data availability. The 2011 Release is the largest since the year 2000 with all 29 areas located in Commonwealth waters offshore NT, WA, Victoria and Tasmania, covering about 200,000 km2. The producing hydrocarbon prov
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35

Ghori, K. Ameed. "Petroleum data: leading the search for geothermal resources in Western Australia." APPEA Journal 49, no. 1 (2009): 365. http://dx.doi.org/10.1071/aj08022.

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In Western Australian basins, subsurface drill-hole data, primarily from petroleum exploration, allows the identification of regions of high temperature at depth that may be potential geothermal resources. The extent and economic viability of such resources remain poorly known and require further study. Observed temperatures at depths up to 4.5 km reach 150°C in parts of the Canning, Carnarvon and Perth basins, indicating low-enthalpy resources related to regional heat flow. The greatest potential for hydrothermal resources is in the Perth Basin where subsurface temperatures of 65–85°C are rea
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36

Graham, E. D. "DRIVERS FOR THE DEVELOPMENT OF AN INTEGRATED SUPPLY BASE AND OFFSHORE SUPPLY CHAIN, NORTH WEST SHELF, AUSTRALIA." APPEA Journal 44, no. 1 (2004): 593. http://dx.doi.org/10.1071/aj03027.

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Since the commencement of the major developments on the North West Shelf, the offshore resource industry, during both its construction and operational phases, has faced considerable logistical impediments to cost-effective solutions for the offshore supply chain. These impediments have included distance, scant resources, lack of infrastructure both on and offshore and lack of critical mass.Throughout the world, offshore projects have greatly benefitted from the availability of integrated services to cater for the transport of equipment from the point of manufacture or distribution to the offsh
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37

Kear, B. P., J. A. Long, and J. E. Martin. "A review of Australian mosasaur occurrences." Netherlands Journal of Geosciences 84, no. 3 (September 2005): 307–13. http://dx.doi.org/10.1017/s0016774600021089.

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AbstractMosasaurs are rare in Australia with fragmentary specimens known only from the Cenomanian-lower Turonian Molecap Greensand (Perth Basin), Campanian - lower Maastrichtian Korojon Calcarenite (Carnarvon Basin), and upper Maastrichtian Miria Formation (Carnarvon Basin), Western Australia. These units were laid down during a near-continuous marine inundation of the western margin of the Australian landmass (which followed separation from India in the Valanginian and genesis of the Indian Ocean) in the Early-Late Cretaceous. The Australian mosasaur record incorporates evidence of derived mo
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38

Jurinak, Jeff, and Bruce Anderson. "2012 PESA production and development review." APPEA Journal 53, no. 1 (2013): 165. http://dx.doi.org/10.1071/aj12013.

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2012 was a pivotal year for Australian petroleum development and production, during a dynamic time in our region, and globally. Australian activity headlines are LNG, the continuing pace and scale of the development of major projects, and record national petroleum production. LNG development in Australia is proceeding apace, with seven sanctioned projects under construction in WA and Queensland. The scale of the major projects underway is being felt with competition for skills, materials and services driving cost inflationary pressures and, coupled with other factors—such as an historically hi
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39

Carpenter, Chris. "Early Production Life of Wheatstone Project Offshore Australia Yields Key Lessons." Journal of Petroleum Technology 73, no. 08 (August 1, 2021): 51–52. http://dx.doi.org/10.2118/0821-0051-jpt.

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This article, written by JPT Technology Editor Chris Carpenter, contains highlights of paper SPE 202246, “Wheatstone: What We Have Learned in Early Production Life,” by John Pescod, SPE, Paul Connell, SPE, and Zhi Xia, Chevron, et al., prepared for the 2020 SPE Asia Pacific Oil and Gas Conference and Exhibition, originally scheduled to be held in Perth, Australia, 20–22 October. The paper has not been peer reviewed. Wheatstone and Iago gas fields, part of the larger Wheatstone project, commenced production in June 2017. The foundation subsea system includes nine Wheatstone and Iago development
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40

Bradshaw, Marita. "Review of the 2008 offshore petroleum exploration release areas." APPEA Journal 48, no. 1 (2008): 359. http://dx.doi.org/10.1071/aj07025.

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Each year the Australian Government releases new offshore opportunities for petroleum exploration. Thirty-five new exploration areas located across five of Australia’s offshore sedimentary basins are offered in the 2008 Release. All the areas are available through a work program bidding system with closing dates for bids at six and 12 months from the date of release. Acreage in the first round closes on 9 October 2008 and includes the more explored areas. The second closing round on 9 April 2009 comprises acreage located in less well explored and frontier regions. The 2008 exploration areas ar
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41

T, T., S. Loutit, K. K. Romine, and C. B. Foster. "SEQUENCE BIOSTRATIGRAPHY, PETROLEUM EXPLORATION AND A. CINCTUM." APPEA Journal 37, no. 1 (1997): 272. http://dx.doi.org/10.1071/aj96017.

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Sequence biostratigraphy is a relatively new discipline that has rapidly expanded in parallel with the development of sequence stratigraphy. Sequence bios- tratigraphic concepts have resulted in significant improvements in our ability to calibrate biozones, correlate and determine ages of sedimentary units, and to estimate environments of deposition. Significant advances in the development of integrated biostratigraphic methods and knowledge during the past 20 years are now being rapidly integrated into the physical framework provided by depositional sequences. Sequence stratigraphy provides a
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42

Krassay, Andrew, Jane Blevin, and Donna Cathro. "Exploration highlights for 2007." APPEA Journal 48, no. 1 (2008): 395. http://dx.doi.org/10.1071/aj07028.

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Record-high oil prices along with on-going development of infrastructure, increasing domestic demand and international LNG sales continued to drive significant investment in exploration in onshore and offshore Australia during 2007. These trends are reflected nationally by strong uptake of acreage and continued high levels of drilling activity and seismic acquisition. Overall, drilling and discovery trends were similar to 2006 which showed significant exploration activity focussed on proven hydrocarbon basins (Carnarvon, Browse, Perth and Cooper basins). Most petroleum discoveries made in 2007
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43

DOUGHTY, PAUL, LUKE KEALLEY, and JANE MELVILLE. "Taxonomic assessment of Diporiphora (Reptilia: Agamidae) dragon lizards from the western arid zone of Australia." Zootaxa 3518, no. 1 (October 16, 2012): 1. http://dx.doi.org/10.11646/zootaxa.3518.1.1.

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Members of the genus Diporiphora are slender perching agamid lizards from Australasia, with a conservative morphologyand some outstanding taxonomic issues. Here we assess morphological variation in the morphologically similar D. pin-dan, D. valens, and D. winneckei from the western deserts of Australia. A reassessment of morphological differences thatincluded the presence or absence of a gular fold, revealed D. pindan to be much more widely distributed than previouslythought, occurring as far south as the northern Pilbara and east to the Tanami Desert. Examination of D. valens specimensreveale
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44

Bernecker, Thomas. "A petroleum geological overview of the 2013 offshore acreage release for petroleum exploration." APPEA Journal 53, no. 1 (2013): 69. http://dx.doi.org/10.1071/aj12007.

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The Australian Government formally releases new offshore exploration areas at the annual APPEA conference. The previous two releases were characterised by several large, gazetted areas in underexplored regions, a trend that is maintained this year with several frontier areas comprising more than 100 graticular blocks on offer. The recent uptake of new exploration permits in the Bight Basin, the offshore North Perth Basin, and the Roebuck Basin indicates a continuing strong industry interest in offshore frontier exploration. A total of 31 areas in 13 geological provinces are formally released i
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45

Pryer, Lynn, Jane Blevin, Gabriel Nelson, Guillaume Sanchez, Jen-Deng Lee, Donna Cathro, Rod Graham, and Brian Horn. "Structural architecture and basin evaluation of the North West Shelf." APPEA Journal 54, no. 2 (2014): 474. http://dx.doi.org/10.1071/aj13047.

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The WestraliaSPAN 2D regional program extends across all basins of Australia’s North West Shelf (Carnarvon/Roebuck/Browse/Bonaparte basins) and Arafura regions. The survey is designed with long offset and record length (18 sec) acquisition parameters to image the important deep crustal and sub crustal architecture and depositional systems across this complex margin. The regional program provides unique, state-of-the-art depth imaging of deep-basement rift structures of the Westralian Superbasin, as well as the lower crust and Moho. The survey has multiple transects which cross the transition f
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46

Southgate, Peter, Keith Sircombe, and Christopher Lewis. "New insights into reservoir sand provenance in the Exmouth Plateau and Browse Basin." APPEA Journal 51, no. 2 (2011): 715. http://dx.doi.org/10.1071/aj10095.

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A pilot study to determine if zircons present in reservoir facies of the North West Shelf can be used to identify provenance and sediment transport pathways has analysed samples from three wells: Guardian–1 and Hijinx–1 (Carnarvon Basin), and Burnside–1 (Browse Basin). Operating companies Chevron, Santos and Hess collected 3–5 kg of cuttings from sandstone bodies intersected in the three wells. Samples were sent to Geoscience Australia for zircon separation and analysis at the Geochronology Laboratory on a sensitive high-resolution ion microprobe (SHRIMP). To provide a statistically meaningful
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47

Dettmann, Mary E., and David M. Jarzen. "Pollen evidence for Late Cretaceous differentiation of Proteaceae in southern polar forests." Canadian Journal of Botany 69, no. 4 (April 1, 1991): 901–6. http://dx.doi.org/10.1139/b91-116.

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Amongst diverse and abundant fossil proteaceous pollen in southeastern Australian Late Cretaceous (Campanian–Maastrichtian) sediments are forms identical with pollen of extant taxa within subfamilies Proteoideae, Persoonioideae, Carnarvonioideae, and Grevilleoideae. Taxa identified now have disparate geographic ranges within Australasia. Sclerophyllous Adenanthos and Stirlingia (Proteoideae) are restricted to the southern Australian Mediterranean climatic region; Persoonia (Persoonioideae) ranges into higher rainfall areas of eastern and northern Australia. Grevillea exul – Grevillea robusta a
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48

Bernecker, Thomas. "Review of the 2009 offshore petroleum exploration release areas." APPEA Journal 49, no. 1 (2009): 465. http://dx.doi.org/10.1071/aj08031.

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The Australian Government formally releases new offshore exploration areas at the annual APPEA conference. This year, 31 areas plus two special areas in five offshore basins are being released for work program bidding. Closing dates for bid submissions are either six or twelve months after the release date (i.e. 3 December 2009 and 29 April 2010), depending on the exploration status in these areas is and on data availability. The 2009 release areas are located in Commonwealth waters offshore Northern Territory, Western Australia, South Australia and Victoria, comprising intensively explored ar
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49

Dettmann, Mary E., and David M. Jarzen. "The Early History of the Proteaceae in Australia: the Pollen Record." Australian Systematic Botany 11, no. 4 (1998): 401. http://dx.doi.org/10.1071/sb97022.

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The early history of the Proteaceae in Australia is traced from the record of fossil pollen that possess characters having taxonomic resolution among extant members of the family. Pollen characters useful for segregating subfamilies and generic groups are apertural number and form together with exine stratification and structure. When considered in conjunction with pollen shape, polarity, and size and exine sculpturing, they may be used to discriminate generic and/or species groups. The fossil pollen record suggests that the family originated in northern Gondwana during the late Cenomanian and
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50

Fredericks, Bronwyn, and Abraham Bradfield. "Revealing and Revelling in the Floods on Country: Memory Poles within Toonooba." M/C Journal 23, no. 4 (August 12, 2020). http://dx.doi.org/10.5204/mcj.1650.

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In 2013, the Capricornia Arts Mob (CAM), an Indigenous collective of artists situated in Rockhampton, central Queensland, Australia, successfully tendered for one of three public art projects that were grouped under the title Flood Markers (Roberts; Roberts and Mackay; Robinson and Mackay). Commissioned as part of the Queensland Government's Community Development and Engagement Initiative, Flood Markers aims to increase awareness of Rockhampton’s history, with particular focus on the Fitzroy River and the phenomena of flooding. Honouring Land Connections is CAM’s contribution to the project an
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