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http://www.gfz-potsdam.de/portal/gfz/Struktur/Departments/Department+4/sec43 Vision - to address the exploration, production, environmental ramifications and public acceptance of shale gas exploitation in SA Partners – GFZ-AEON, South African universities, South African government institutions, international and national energy companies Steering Committee - GFZ-AEON, each industry sponsor, PASA in advisory role Introduction The last few years have seen important developments in alternative exploration plays related to energy. One of these is Shale Gas which, along with tight gas sands and coalbed methane, has emerged as a new major gas resource in the lower 48 states of the USA over the last 10 years, and is now expanding into Europe ( www.gas-shales.org ) and elsewhere.Annual natural gas production from shale gas reservoirs in the US is approximately 1.0 Tcf and comes from more than 40,000 shale gas wells (around 6-10% of total natural-gas production in the US today; numbers vary according to reference). As far as Africa is concerned, sub-Saharan shale gas has been estimated at 300 Tcf, and South Africa’s highest potential is concentrated in the Karoo Basin. Exploration of the Karoo Basin started in the early 20th century. During the 1960’s to early 1970’s, seismic data was acquired and about 25 exploration wells were drilled with very limited success within the proposed study area which covers the southern part of the Karoo Basin. Dry holes were attributed to low productivities of the tight Paleozoic reservoirs and drilling problems were associated with the high density of Jurassic intrusions. |
Exploration in the southern part of the Karoo Basin effectively ceased during the late 1970’s. At present, new insights into unlocking the potential of tight conventional and unconventional reservoirs, combined with new drilling and completion technologies might be successfully applied in the southern part of the Karoo Basin. Initial 3-year focus will be on building a GEODATABASE - content defined by steering committee - located at UCT/AEON with web access - PASA to provide maps and logs as per their regulations - published data to be collated, tabulated and archived - samples from the field and cores/cuttings to be collected - shallow drilling vital because shales poorly outcropped and weathered - analyses to be performed to address gas-in-place and fracturability - analyses to be performed by service companies at low cost - new analytical data to be entered into the database on regular basis - specialised analyses may follow, as decided by steering committee - database remains proprietary for 2 years after conclusion of project - database content forms basis of MSc and PhD studies - results must be published but with filter as to timing. |
Ref. Sub-Project (Theme)
POST-GONDWANA TECTONICS FROM NAMAQUALAND TO THE KALAHARI
Under investigation:
Benefits:
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Sub-Project |
Post-Gondwana tectonics in western South Africa: from the Namaqualand offshore to the Kalahari - Implications for hydrocarbon exploitation, mineral exploration and seismic risk mitigation |
Core participants (* indicates project coordinator; ^ indicates postgraduate student, contract researcher)
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GeoForschungsZentrum (GFZ)
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Oliver Heidbach |
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South African Nuclear Energy Corporation (Necsa), SA |
Marco Andreoli* (UW) |
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Namib Geovista (NG) –
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Zvi Ben-Avraham |
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University Stellenbosch (US), SA |
Cathy Clarke-Dowding Olwethu Majodina^ |
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Mike Watkeys Saumitra Misra |
| Hartebeesthoek Radio Astronomy Observatory (HartRAO) - Space Geodesy Programme (SA) | Ludwig Combrinck |
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University of the
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Summary
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The end of the
Jurassic, at ~144 Ma, is accompanied in southern Gondwana by the
developing rift along the site of the future south Atlantic. Another
major event took place at that time in what became the South African
sector of the Kalahari basin, namely the impact of the giant Morokweng
meteorite. This impact arguably produced the third largest crater in
the terrestrial record, releasing the vertical tectonic stresses
responsible for the rise of the ~240 km Morokweng/Ganyesa dome structure
and the emplacement of basaltic dykes. As Africa and
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2010/05/16 12:07:44 PM