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Deep Mantle Recycling Revealed in Diamonds and their Mineral Inclusions (NERC Grant NE/J008583/1)

Three Published Papers; Thomson et al CMP 2014 - Origin of Sub-Lithospheric diamonds from the Juina-5 Kimberlite (Brazil): constraints from Carbon Isotopes and Inclusion Compositions...

Orogenic Plateau Magmatism (NERC grant NE/H021620/1)

This dataset contains major element, trace element and isotopic analyses for samples collected during the NERC project "Orogenic Plateau Magmatism" (NE/H021620/1) (2011-2014). Samples are late...

Azores processed theoretical waveforms (NERC grant NE/N011791/1)

Theoretical waveforms computed to study earthquakes in the Azores archipelago. Grant abstract: How do earthquakes happen? Understanding the nature of earthquakes is a key fundamental question in...

Processed SAR interferograms (NERC grant NE/N011791/1)

Processed SAR interferograms for the Wells, Nevada earthquake. Grant abstract: How do earthquakes happen? Understanding the nature of earthquakes is a key fundamental question in Geociences that...

Fe isotope data constraining the evolution of the Galápagos mantle plume (NERC Grant NE/V000411/1)

The data consists of Fe-isotope ratio measurements, expressed in permil notation (δ57Fe) relative to the international standard IRMM-014 following standard practise. The measurements are of bulk...

Chemical analysis data derived from NERC grant NE/I025573/1, When on Earth did modern plate tectonics begin?

Earth is a dynamic planet, for the simple reason that it is still cooling down from the heat of accretion and subsequent decay of radioactive elements. The main mechanism by which it loses heat is...