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Basement dykes in Panafrican crust, Sinai Peninsula

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ArcGIS REST API: ColorScheme

Needed to look up ArcGIS's JSON color settings as served by the REST API. So it is listed on their Common Data Types -> Symbol objects and they indeed use RGBA.

To quote from ESRI's website:

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2018/09/24 15:07 · christian · 0 Comments

IODP Expedition 388: Equatorial Atlantic Gateway

Our IODP proposal, led by Tom Dunkley-Jones, to drill the Equatorial Atlantic, off the Brazilian Pernambuco Plateau has been successful and is now scheduled to sail in August/September 2020 as IODP Expedition 388 "Equatorial Atlantic Gateway".

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2018/07/17 14:09 · christian · 0 Comments

From the dusty archives

While cleaning up some of my hard drives I came across an old PLATES data type code specification as simple text file. Now linked here

2018/05/27 20:01 · christian · 0 Comments

Short course in Basin Analysis at LMU

Someone has landed in front of the Neue Pinakothek

The “southern” version of the Exploration Tectonics/Basin Analysis course successfully took place at the Ludwigs-Maximilans Uni in Munich over the past three days, generously hosted by HP Bunge in the Geophysics department.

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New paper out - Crustal Structure of the Andean Foreland in Northern Argentina: Results from Data-integrative Three-dimensional Density Modeling

I am co-author on a paper by Christian Meeßen (GFZ) investigating the crustal structure of the Andean foreland in Argentina. The paper is published in J. Geophys. Research, currently in “Early View” - Here's the abstract:

Previous thermomechanical modeling studies indicated that variations in the temperature and strength of the crystalline crust might be responsible for the juxtaposition of domains with thin-skinned and thick-skinned crustal deformation along strike the foreland of the central Andes. However, there is no evidence supporting this hypothesis from data-integrative models. We aim to derive the density structure of the lithosphere by means of integrated 3-D density modeling, in order to provide a new basis for discussions of compositional variations within the crust and for future thermal and rheological modeling studies. Therefore, we utilize available geological and geophysical data to obtain a structural and density model of the uppermost 200 km of the Earth. The derived model is consistent with the observed Bouguer gravity field. Our results indicate that the crystalline crust in northern Argentina can be represented by a lighter upper crust (2,800 kg/m3) and a denser lower crust (3,100 kg/m3). We find new evidence for high bulk crustal densities >3,000 kg/m3 in the northern Pampia terrane. These could originate from subducted Puncoviscana wackes or pelites that ponded to the base of the crystalline crust in the late Proterozoic or indicate increasing bulk content of mafic material. The precise composition of the northern foreland crust, whether mafic or felsic, has significant implications for further thermomechanical models and the rheological behavior of the lithosphere. A detailed sensitivity analysis of the input parameters indicates that the model results are robust with respect to the given uncertainties of the input data.

Citation: Meeßen, C., Sippel, J., Scheck-Wenderoth, M., Heine, C., & Strecker, M. R. (2018). Crustal structure of the Andean foreland in northern Argentina: Results from data-integrative three-dimensional density modeling. Journal of Geophysical Research: Solid Earth, 123. Doi:10.1002/2017JB014296

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