35TH INTERNATIONAL GEOLOGICAL CONGRESS

35TH INTERNATIONAL GEOLOGICAL CONGRESS

27 AUGUST - 4 SEPTEMBER 2016  |  CAPE TOWN, SOUTH AFRICA


Sponsors

Keystone Sponsor Exxaro
Diamond Sponsor Vale
Gold Sponsor Vale
Silver Sponsor Bushveld Minerals Randgold VM Investment Company Bauer
Business Centre Sponsor Chamber of Mines
Publication Sponsor Acacia mining VM Investment Company
Social Function
Nedbank
Plenary Speaker Sponsor
Speaker Gift Sponsor
Post Graduate Fund
Registration
Welcome Drinks
Lunch Time Drinks
Publication &
35 IGC SAGPGF
Pangea Exploration (Proprietary) Limited
35 IGC SAGPGF
MY IGC APP
Symposium Sponsor
Audit Sponsor

Partners

IUGS GSSA Department of Mineral Resouces Council for Geoscience UNESCO Department of Science and Technology National Research Foundation AGU International and Domestic Airline Partner Cape Town & Western Cape Convention Bureau Emirates National Convention Bureau Creamer Media Mining Weekly

35TH INTERNATIONAL GEOLOGICAL CONGRESS

27 AUGUST - 4 SEPTEMBER 2016  |  CAPE TOWN, SOUTH AFRICA

Pre 7 Eastern Limb of the Bushveld Complex

The 2.055 Ga–old Bushveld Complex is situated in the north-eastern part of South Africa.  Three distinct groups of rocks make up the Complex but this excursion is directed primarily at the layered ultramafic-mafic rocks.  We will, however, briefly examine the roof rocks, the older felsite and younger granite and granophyre, as well as the floor rocks, metasediments of the Transvaal Supergroup and Bushveld sills. The eastern limb reveals spectacular outcrops which are ascribed to the uplift and subsequent erosion of the interior plateau of southern Africa.

The excursion will encompass the five zones into which the layered sequence is subdivided.  The Critical Zone is emphasized as this is where layering is most intricate and where many of the mineralized reefs occur.   Underground and surface visits to chromite and platinum mines are envisaged, as well as historical declines on the Merensky Reef close to the discovery site.  Field traverses of the chromitite layers are a highlight, as is Dwarsrivier where layers of chromitite and anorthosite are superbly exposed.  The uniquely zoned Driekop and Onverwacht pipes and a discordant body of iron-rich ultramafic pegmatite complete some of the unusual features of the Critical Zone.

Traverses of the Lower Zone to examine layers of dunite, harzburgite and bronzitites, as well as of layers of Ti-magnetite, anorthosite, and ferrogabbro in the Upper Zone are also included, as is an opportunity to examine some of the more discrete layering of the Main Zone.

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Field Trip Leader: Roger Scoon                                                                        
Start/End: OR TAMBO International Airport Johannesburg
Departs: 
09:00 AM
Dates: 6 days, Monday 22nd to Saturday 27th August 2016                     
Price: R 14 850 per person sharing with single supplement of R 5 850 per person

Info from Trip Leader

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