Matt Fox joins the LGC
The provenance of Taklamakan desert sand
Rittner, M., Vermeesch, P., Carter, A., Bird, A., Stevens, T., Garzanti, E., Andò, S., Vezzoli, G., Dutt, R., Xu, Z., Lu, H., 2016. The provenance of Taklamakan desert sand. Earth Planet. Sci. Lett. 437, 127–137. doi:10.1016/j.epsl.2015.12.036
New paper in Chemical Geology
There is a lot to do on the Internet about the concept of 'Big Data', in which huge online databases are 'mined' to reveal previously hidden trends and relationships in society. One could argue that sedimentary geology has entered a similar era of 'Big Data', as modern provenance studies routinely use multiple proxies to dozens of samples, resulting in large multivariate datasets comprising thousands of data points. Just like the Internet, sedimentary geology now requires specialised statistical tools to visualise and interpret such large datasets. Pieter Vermeesch (LGC) and Eduardo Garzanti (University of Milan - Bicocca) introduce 3-way multidimensional scaling and Procrustes analysis as simple yet powerful tools to achieve this goal. Reference: Vermeesch, P. and Garzanti, E., 2015, Making geological sense 'Big Data' in sedimentary provenance analysis. Chemical Geology, doi:10.1016/j.chemgeo.2015.05.004, v.409, 20-27 |
Leverhulme grant to study the history of the Milky Way

A £174,468 grant entitled Assessing the potential of lunar geology as a window into galactic history, was awarded by the Leverhulme Trust to Professor Crawford (Birkbeck College) and colleagues Dr Pieter Vermeesch (UCL) and Dr Katherine Joy (University of Manchester). Dr Louise Alexander (Birkbeck) will be employed as a postdoctoral researcher on the grant, and will carry out cosmogenic 3He, 21Ne and 38Ar at the LGC, in order to find out what the Moon may tell us about the history of the Milky Way Galaxy.
QEMSCAN @ LGC
Facilitated by the UCL Corporate Partnerships team, the LGC has teamed up with Rocktype Ltd. to host a FEI’s QEMSCAN® WellSite™. Rocktype's co-founder and Chief Geologist Dr. Jenny Omma will join the LGC as an honorary member of staff.
The QEMSCAN WellSite technology is a high-resolution scanning electron microscope (SEM) that enables the detection, classification and quantitative analysis of mineralogy and lithology utilising energy-dispersive X-ray spectrometers. The combination of QEMSCAN with the LGC’s existing LA-ICP-MS facilities creates a new instrument suite capable of fingerprinting sediments with high resolution and speed. In addition, the ruggedised nature of the QEMSCAN WellSite provides a robust, field-reliable platform that Rocktype will use to rapidly analyse chemical and rock properties to calibrate well logs and more accurately predict matrix density.
This new capability we enable exciting new applications in petrophysical modelling, basin modelling, reservoir quality assessment and sedimentary provenance studies.
Further information about the collaboration can be found in this press release
The QEMSCAN WellSite technology is a high-resolution scanning electron microscope (SEM) that enables the detection, classification and quantitative analysis of mineralogy and lithology utilising energy-dispersive X-ray spectrometers. The combination of QEMSCAN with the LGC’s existing LA-ICP-MS facilities creates a new instrument suite capable of fingerprinting sediments with high resolution and speed. In addition, the ruggedised nature of the QEMSCAN WellSite provides a robust, field-reliable platform that Rocktype will use to rapidly analyse chemical and rock properties to calibrate well logs and more accurately predict matrix density.
This new capability we enable exciting new applications in petrophysical modelling, basin modelling, reservoir quality assessment and sedimentary provenance studies.
Further information about the collaboration can be found in this press release
New paper in JAAS
A new paper by James documents an isobaric interference on 4He, which affects in-situ U-Th-He measurements on young and U-Th-poor samples. This interference varies with trap current and filament voltage but can be corrected for by monitoring double-charged carbon.
Reference: Schwanethal, J., 2015, Minimising 12C3+ interference on 4He+ measurements in a noble gas mass spectrometer, J. Anal. At. Spectrom. DOI: 10.1039/C4JA00422A
GRL features Yuntao Tian's latest paper on its cover

In his latest paper, Yuntao (in collaboration with colleagues in Australia and China) has used the apatite fission track method to reveal a Miocene phase of rapid cooling in the eastern Tibetan crust. This cooling event is attributed to synchronous river incision, consistent with regional surface uplift generated by crustal extrusion along a detachment at depth.
Tian, Yuntao, et al. "Synchronous fluvial response to surface uplift in the eastern Tibetan Plateau: Implications for crustal dynamics." Geophysical Research Letters (2015).