Geochemical and mineralogical changes in a coal seam due to contact metamorphism, Sydney Basin, New South Wales, Australia

1989 ◽  
Vol 11 (2) ◽  
pp. 105-125 ◽  
Author(s):  
Colin R. Ward ◽  
Peter R. Warbrooke ◽  
F. Ivor Roberts
Author(s):  
R. A. Binns

SummaryWith progressive increase in grade of contact metamorphism, aluminous hornblendes in some New England basic hornfelses change from a pale blue-green variety with ragged actinolitic habit, to a deeper bluish-green variety, then to a deeply coloured brownish type with granular habit. At all stages the coexisting plagioclase is appreciably calcic. No outer aureole of albite-epidote-actinolite hornfels has been recognized. The higher grade hornblendes are richer in alkalis and titanium, and poorer in octahedrally co-ordinated aluminium than those formed at low grades. Two analysed hornblendes display an unusual excess of calcium, which occupies the Y site, and another has a very high content of ferrous iron and potassium.


Clay Minerals ◽  
1971 ◽  
Vol 9 (1) ◽  
pp. 107-123 ◽  
Author(s):  
J. D. Hamilton

AbstractThe minus 1μm fraction of an argillized vitric tuff, overlying the Wallarah Coal Seam near Swansea, N.S.W. is a nearly monomineralic (95%+) expandite clay, which hydrates and reacts to glycerol and heat treatments like montmorillonite. Results of X-ray, differential thermal, thermogravimetric and infrared absorption analyses confirm the general montmorillonoid character of the mineral, but chemical data indicate that much of its structure charge arises from substitutions in the tetrahedral zones of the lattice, as in beidellite rather than montmorillonite. The structural fOrmula deduced for the Ca++-saturated form of the minus 0.1μm clay is:The distinctive behaviours of the heat-treated NH4+- and Li+-saturated structures also suggest that the mineral is a 'beidellitic montmorillonite' rather than a montmorillonite.


2020 ◽  
pp. 65-89
Author(s):  
Carolyn M. Hendriks ◽  
Selen A. Ercan ◽  
John Boswell

Chapter 4 presents an empirical case on the problematic public disconnect in contemporary democracy where multiple publics are fractured in the public sphere. The chapter explores how a group of everyday citizens created connections between diverse publics in the public sphere. The analysis centres on the creative and playful connective activities of Knitting Nannas Against Gas (KNAG), an Australian-based social protest group opposed to coal seam gas development. Drawing on interviews conducted with the members of these groups across four different locations in New South Wales, the chapter reveals a rich variety of ways in which these groups seek to create connections with two opposing publics, as well as with latent publics. The chapter shows the significance of aesthetic-affective forms of communication, including non-verbal communication in crafting novel connections in a fractured public sphere, and discusses the ways these connections can help enhance the epistemic quality and reflexivity of the public sphere. The chapter concludes by discussing how the case of KNAG enriches current ideas on connectivity in deliberative systems.


2017 ◽  
Vol 57 (2) ◽  
pp. 549 ◽  
Author(s):  
David Snashall ◽  
Sabrina Genter

The coal seam gas (CSG) industry in New South Wales (NSW) has reached a stalemate, despite a growing demand for domestic gas. The present paper suggests that a key reason for this is the industry’s loss of its social licence to operate, which resulted from a loss in trust and a lack of perceived procedural fairness.


1935 ◽  
Vol 72 (9) ◽  
pp. 385-400 ◽  
Author(s):  
Germaine A. Joplin

Recently an account of the endogenous contact-zone of the non-magnesian limestones at Ben Bullen was published in this Magazine (Joplin, 1935 a), and it is now proposed to examine the effects of normal contact metamorphism in the aureole of the Ben Bullen plutonic complex.


2009 ◽  
Vol 49 (1) ◽  
pp. 79 ◽  
Author(s):  
G. Baker ◽  
S. Slater

The commercial production of coal seam gas (CSG) in Australia commenced in 1996. Since then its production has grown up significantly, particularly in the last five years, to become an integral part of the upstream gas industry in eastern Australia. The major growth in both CSG reserves and production has been in the Bowen and Surat basins in Queensland. Active exploration and appraisal programs with the first pilot operations were established in the Galilee Basin in 2008; however, an important reserve base has been built up in New South Wales in the Clarence-Moreton, Gloucester, Gunnedah and Sydney basins. There has been modest CSG production from the Sydney Basin for some years with commercial production expected to commence in the other three basins by or during 2010. Exploration for CSG has been undertaken in Victoria and Tasmania while programs are being developed in South Australia focussing on the Arckaringa Basin. Elsewhere in Australia planning is being undertaken for CSG exploration programs for the Pedirka Basin in the Northern Territory and the Perth Basin in Western Australia. CSG was being supplied into the eastern Australian natural gas market at 31 December 2008 at a rate of approximately 458 TJ per day (167 PJ per year). Queensland is currently producing 96.7% of this total. Approximately 88% of the natural gas used in Queensland is CSG. Currently, CSG accounts for nearly 25% of the eastern Australian natural gas market, estimated at 670 PJ per year. The production of CSG is now a mature activity that has achieved commercial acceptability, especially for coal seam derived gas from the Bowen and Surat basins. The recent proposals by a number of local CSG producers—in joint venture arrangements with major international groups—to produce liquefied natural gas (LNG) from CSG along with a number of merger and acquisition proposals, is testimony to the growing economic and commercial significance of the CSG sector. Should all of the proposed CSG based LNG projects eventuate, LNG output would be approximately 40 million tones per year. This will require raw CSG production to increase to approximately 2,600 PJ per year, resulting in a four fold increase from the present natural gas consumption in eastern Australia. The proved and probable (2P) reserves of CSG in eastern Australia at 31 December 2008 were 17,011 PJ or 60.2% of the total independently audited 2P natural gas reserves of 28,252 PJ. The Bowen and Surat basins with 16,120 PJ have the largest onshore gas reserves eastern Australia. In New South Wales, the 2P CSG reserves at the end of 2008 were 892 PJ, though this is expected to increase significantly over the next 12 months. Major upstream natural gas producers such as Origin Energy Limited and Santos Limited both hold over 50% of their Australian 2P gas reserves as CSG. The 1P reserves of CSG in eastern Australia at 31 December were reported as 4,197 PJ while the 3P reserves of CSG at the same date were 40,480 PJ. Most companies in the CSG sector are undertaking development work to upgrade their 3P reserves (and contingent resources) into the 2P category. The CSG resource in eastern Australia is very large. Companies with interests in CSG have reported in excess of 200,000 PJ as gas in place in the Bowen, Clarence-Moreton, Galilee, Gloucester, Gunnedah, Queensland Coastal, Surat and Sydney basins. The 2P reserves of CSG are expected to exceed 20,000 PJ by the end of 2009. A significant part of the expected large increase in 2P reserves of gas initially will be dedicated to the proposed LNG projects being considered for Gladstone. The major issues confronting the CSG industry and its rapid growth are concerned with land access, overlapping tenure (particularly in Queensland with underground coal gasification) the management and beneficial use of co-product formation water and gas production ramp up factors associated with the proposed LNG projects.


1991 ◽  
Vol 31 (1) ◽  
pp. 367
Author(s):  
Michael Hill ◽  
Michael Armstrong

The coal seams of the coal basins in New South Wales contain vast resources of methane. The gas has been of interest in the past, principally because the inflow of significant quantities into coal mine workings is a danger to mine safety and reduces production. Drainage techniques have been introduced into deeper collieries but they have not proved to be totally effective.Surface pre-drainage operations using hydraulic fracturing to stimulate gas production have been successful in the United States over recent years. The technique has yet to be successfully tested in New South Wales but if effective it will enable future mining areas to be drained prior to commencement of mining. The technique will also enable commercial production of large quantities of methane from both within and outside the coal mining areas.Seven organisations have commenced or will soon commence the exploration and development of the State's coal seam methane resources. Total planned expenditure over the next two years is over $4 000 000. Other Australian and overseas organisations are actively reviewing investment opportunities.Detailed exploration programs will be required prior to the commencement of operations because of the relative lack of data on the geology and gas resources of the basins. Differences exist between Australian and American coals and comparative reservoir and pilot studies will be required to determine the most effective pre-drainage methods. Potential markets exist in the State for methane and changes have been made to relevant legislation and administrative procedures to create incentives for exploration and production. Careful land-use planning will be required to ensure that the gas resource is not sterilised.


2000 ◽  
Vol 40 (1) ◽  
pp. 751
Author(s):  
P.F. Dighton

Significant work is taking place in Queensland and New South Wales to make the recovery of natural gas from coal seams (Coal Seam Methane) a viable industry. At this stage there are still some daunting hurdles to overcome. Australian buyers and financiers remain sceptical on resource risk and continuity of supply issues. In the USA commercial production has been taking place for 20 years, but the industry was only able to achieve credibility and viability by relying on tax breaks. Unfortunately, the same type of government incentives are not present in Australia. Whether, in the absence of these incentives, Australian producers can harness the resource on an economic basis remains to be seen.


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