Metadata 3202

Zeta potential measurements of the fluorcarbonate mineral parisite-(Ce), under water, supernatant and collector conditions. Zeta potential measurements can be used to indicate the surface behaviour of a mineral under different reagent conditions. Mineral surface behaviour is important in processing and extracting minerals from their host ore, which can be energy intensive. Parisite-(Ce) is a fluorcarbonate mineral which contains rare earth elements. Rare earth elements are important in a wide range of prod...

During the period 1982-86 a team of geologists from the British Geological Survey carried out a programme of regional geological mapping and geochemical exploration in collaboration with the Zimbabwe Geological Survey under a Technical Co-operation agreement supported by the UK Department for International Development (DFID) (formerly Overseas Development Agency). Three regions of Zimbabwe were mapped (Harare, Rushinga & Nyampanda, and Makaha) and the results of the stream sediment geochemical surveys were...

Synchrotron X-radiography (images) and diffraction data collected to measure anelasticity of zinc. NERC grant NE/H016309/1 - Experimental determination of mantle rheology. NERC grant NE/L006898/1 - The strength of the lower mantle.

The harmonized geological map of Slovenia is a simplified version of the 1:250 000 scale Geological Map of Slovenia (Buser, 2009), which was compiled using the Basic Geological Map of Slovenia at a scale of 1: 100.000 (compiled by various authors during the 1960's to 1980's) with the addition of new information by Buser. It is primarily a lithostratigraphic map.The faults were selected for portrayal using two criteria; regional extent and tectonic importance. The map presented here was edited specifically ...

The harmonized geological map of Slovenia is a simplified version of the 1:250 000 scale Geological Map of Slovenia (Buser, 2009), which was compiled using the Basic Geological Map of Slovenia at a scale of 1: 100.000 (compiled by various authors during the 1960's to 1980's)with the addition of new information by Buser. It is primarily a lithostratigraphic map.The faults were selected for portrayal using two criteria; regional extent and tectonic importance.The map presented here was edited specifically fo...

The harmonized geological map of Slovenia is a simplified version of the 1:250 000 scale Geological Map of Slovenia (Buser, 2009), which was compiled using the Basic Geological Map of Slovenia at a scale of 1: 100.000 (compiled by various authors during the 1960's to 1980's) with the addition of new information by Buser. It is primarily a lithostratigraphic map.The faults were selected for portrayal using two criteria; regional extent and tectonic importance. The map presented here was edited specifically ...

The harmonized geological map of Slovenia is a simplified version of the 1:250 000 scale Geological Map of Slovenia (Buser, 2009), which was compiled using the Basic Geological Map of Slovenia at a scale of 1: 100.000 (compiled by various authors during the 1960's to 1980's) with the addition of new information by Buser. The map depicts the lithostratigraphic makeup of Slovenia .The map presented here was edited specifically for the purpose of the OneGeology-Europe project by M. Bavec, M. Novak, M. Poljak,...

The harmonized geological map of Slovenia is a simplified version of the 1:250 000 scale Geological Map of Slovenia (Buser, 2009), which was compiled using the Basic Geological Map of Slovenia at a scale of 1: 100.000 (compiled by various authors during the 1960's to 1980's) with the addition of new information by Buser. It is primarily a lithostratigraphic map.The faults were selected for portrayal using two criteria; regional extent and tectonic importance. The map presented here was edited specifically ...

High resolution geological map of Surice Agimont at a scale of 1:25 000 from the Walloon Region. See http://environnement.wallonie.be/cartosig/cartegeologique/

Radar Interferometry map of the Border of Belgium and Netherlands. The blue colours correspond to positive deformation (uplift) of the ground surface related to the recharge of a mining aquifer.