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Titlebook: Basement Tectonics 9; Australia and Other M. J. Rickard,H. J. Harrington,P. R. Williams Conference proceedings 1992 Springer Science+Busin

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期刊全稱Basement Tectonics 9
期刊簡稱Australia and Other
影響因子2023M. J. Rickard,H. J. Harrington,P. R. Williams
視頻videohttp://file.papertrans.cn/181/180940/180940.mp4
學(xué)科分類Proceedings of the International Conferences on Basement Tectonics
圖書封面Titlebook: Basement Tectonics 9; Australia and Other  M. J. Rickard,H. J. Harrington,P. R. Williams Conference proceedings 1992 Springer Science+Busin
影響因子The Ninth International Conference on Basement Tectonics was held at the Australian National University in Canberra 2-6 July 1990. The opening keynote address was given by Prof. R.W.R. Rutland, Director of the Bureau of Mineral Resources. Other keynote speakers were E.S.T. O‘Driscoll, an Australian consultant, and Prof P. Bankwitz, Central Institute for Physics of the Earth, Potsdam, GDR. Technical sessions were arranged by session conveners on the following five topic- i) The structure of the Australian craton and cover basins; ii) Basement structure of continental regions; iii) Structural patterns and mineral deposits; iv) Techniques for analysing basement structures; v) Structural patterns in oceanic crust. The arrangement of papers for this Proceedings Volume has been simplified. Part 1 deals with Australia, Part 2 with other areas and Part 3 lists the titles of all the papers read at the conference. Abstracts of these papers are available in Geological Society of Australia Abstracts No 26 and may be purchased for $AI0 from the Geological Society of Australia Office, ANA House, 301 George Street, Sydney NSW 2000. Field trips to view aspects of the Lachlan Fold Belt and the Sydn
Pindex Conference proceedings 1992
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The Pine Creek Shear Zone, North of Pine Creek (Northern Territory): Structural Evolution and Experie (PCSZ) north of Pine Creek. The NNWN trend and contrary plunging F1 fold system to the east and west of the PCSZ were the principal factors causing the deformation of the 15°-30° clockwise-inclined foliation in the zone. In the experiments these factors were simulated by complex deformation: simpl
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Elusive Trails in the Basement Labyrinthsement. These breaks can be identified in appropriate compilations of standard Geological, geophysical and Geographic data. Pattern breaks appear both as linear and arcuate (ring) discontinuities, and generally correspond to thresholds of change in the distribution of geological structures, attitude
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An E-W Transect Section through Central Iraq basement of Iraq is hidden below younger rocks, several studies in neighbouring countries have been compiled by Buday and Jassim (1987) who deduced that the basement is metamorphosed and of Precambrian age. The Basement depth was determined from an aeromagnetic survey and is used in this study to c
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