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Ref. Sub-Project    (Theme)                                                                                  

   GASHsa - SHALEGAS in SA

                              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:

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)

GeoForschungsZentrum (GFZ) Potsdam (Germany)

Oliver Heidbach

South African Nuclear Energy Corporation (Necsa), SA

Marco Andreoli*  (UW)
Mbuthokazi Mandaba^

University of Cape Town (UCT), SA

Anton LeRoex                                                                Andrew Logue^ (Necsa)

Namib Geovista (NG) – University of Pretoria (UP), SA

Ingrid Stengel

University of Tel Aviv (UTV) -  (UCT)

Zvi Ben-Avraham

University of Basel (UB), Switzerland

Alex Kounov

University of Trondheim (UT)  - Geological Survey of Norway (GSN)

Giulio Viola

University Stellenbosch (US), SA  

Cathy Clarke-Dowding                                                   Olwethu Majodina^

University of KwaZulu-Natal (UKZN), SA

Mike Watkeys                                                             Saumitra Misra

Hartebeesthoek Radio Astronomy Observatory (HartRAO) - Space Geodesy Programme (SA) Ludwig Combrinck

University of the Witwatersrand (UW), SA

 

Ray Durrheim                                                               Terence McCarthy                                                           Roger Gibson                                                                     Hlompo Malephane^                                                                           S Wela^

Summary

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 America became increasingly separated by an expanding Atlantic ocean, the SE Atlantic escarpment experienced, with time, striking changes in both stress orientation and magnitude reflected in folding and faulting of thrusting, extensional and strike slip character.  These tectonic episodes are recorded not only by the Karoo and Cretaceous deposits in western Namibia and Namaqualand, but also in the offshore Orange and Bredasdorp basins and, onshore, in the northwestern Karoo basin and in the Ghaap Plateau (southwestern Kaapvaal craton).  As such, the study of these Cretaceous to post-Cretaceous tectonic events dovetails with other Inkaba ye Africa projects, and constitutes the background needed to assist in the interpretation of the present day strike slip stress field in western southern Africa.  This NW to NNW oriented, so-called Wegener field is of anomalous intensity, puzzling in orientation and may be responsible for the generally low to moderate seismic activity recorded in the western and northern Cape regions. Apart from the study of the Morokweng structure and its economic implications, much of the currently planned research focuses on the various facets of the Wegener stress anomaly, especially its variability in time and space, and its implications for seismic risk assessment and the optimal exploitation of offshore hydrocarbon resources.  

 

 

 

 

 

 

 

 

 

 

 

2010/05/16 12:07:44 PM