- earthquake and tectonic studies
- Geological and Geophysical Studies Worldwide
- Geological and Geochemical Analysis
- Geological formations and processes
- Seismic Imaging and Inversion Techniques
- Geology and Paleoclimatology Research
- Geological and Tectonic Studies in Latin America
- Geological and Geophysical Studies
- High-pressure geophysics and materials
- Research Data Management Practices
- Scientific Computing and Data Management
- Maritime and Coastal Archaeology
- Seismology and Earthquake Studies
- Public Procurement and Policy
- Law, AI, and Intellectual Property
- Seismic Waves and Analysis
- Innovation Policy and R&D
- Auction Theory and Applications
- Archaeological and Geological Studies
Institute of Natural Sciences
2023-2024
Universitätsbibliothek Johann Christian Senckenberg
2024
Muséum national d'Histoire naturelle
2024
Meise Botanic Garden
2023
University College Dublin
2020-2022
Irish Centre for Research in Applied Geosciences
2022
University of Birmingham
2017-2019
Université de Lille
2014-2018
Laboratoire d’Océanologie et de Géosciences
2018
Centre National de la Recherche Scientifique
2014-2018
Continental hyperextension during magma-poor rifting at the Deep Galicia Margin is characterized by a complex pattern of faulting, thin continental fault blocks and serpentinization, with local exhumation, mantle peridotites along S-reflector, interpreted as detachment surface. In order to understand fully evolution these features, it important image seismically structure model velocity greatest resolution possible. Traveltime tomography models have revealed long-wavelength this...
The Distributed System of Scientific Collections (DiSSCo) is a pan-European Research Infrastructure (RI) initiative. DiSSCo aims to bring together natural science collections from 175 museums, botanical gardens, universities and research institutes across 23 countries in distributed infrastructure that makes these physically digitally open accessible for all forms innovation. RI entered the ESFRI roadmap 2018 successfully concluded its Preparatory Phase early 2023. now transitioning towards...
Abstract Low‐angle detachments are fundamental crustal structures found in many extensional systems and plate tectonic boundaries, including onshore basins, rifted margins mid‐oceanic ridges. Direct observations of the complete geometry rare so that aspects our understanding their development evolution rely mainly on proxy numerical simulations. A high‐resolution 3D seismic reflection survey Offshore West Ireland images a corrugated detachment, from its steep oceanward breakaway faults to...
Abstract High‐resolution velocity models developed using full‐waveform inversion (FWI) can image fine details of the nature and structure subsurface. Using a 3D FWI model hyper‐thinned crust at Deep Galicia Margin (DGM) west Iberia, we constrain this margin by comparing its with those in other similar tectonic settings. Velocities representative both upper lower continental are present, but there is no clear evidence for distinct crustal layers within crust. Our supports exhumation under...
A key consideration during the preparatory phase project DiSSCo Prepare – which laid foundations for future Research Infrastructure (Distributed System of Scientific Collections) was need to establish a small number alternative viable financial contribution models and scalable formula could be presented potential funders, with view obtaining minimum necessary operate, as well considering how RI grow increased national funding. This report briefly explains ERIC funding framework chosen its...
Abstract. The first International Ocean Discovery Program (IODP) Core-Log-Seismic Integration at Sea (CLSI@Sea) workshop, held in January–February 2018, brought together an international, multidisciplinary team of 14 early-career scientists and a group scientific mentors specialized subduction zone processes the Nankai Trough, one Earth's most active plate-subduction zones located off southwestern coast Japan. goal workshop was to leverage existing core, log, seismic data previously acquired...
<p>The hyper-extended Porcupine Basin, offshore southwest Ireland, is a component of the Eastern North Atlantic rifted continental margin. The basin developed following multiple rifting phases with different extension directions between Late-Palaeozoic and Cenozoic. present-day north-south trend Basin during main Middle-Jurassic to Lower-Cretaceous phase, which interpreted have overprinted earlier directions. In this study, we outline tectono-stratigraphic architecture...
Mechanisms and sources of funding for European Research Infrastructure Consortiums (ERICs) are diverse, complex can be challenging to identify use. This paper provides a roadmap & Development (R&D) within the pre-commercial procurement (PCP) framework landscape ERICs available from Union with perspective on other tracks funding. Our objective is offer starting point underline opportunities challenges, existing future ERICs. The work presented in this results research carried-out...
<p>We investigate the structures of hyper-extended continental crust and 3D nature development syn-rift fault networks at Galicia margin, West Spain, based on observations from a multi-channel seismic reflection dataset acquired in 2013. This volume provides, for first time, high-resolution imaging network geometry above detachment (The “S reflector”) distal setting margin. The margin is sediment-starved, magma-poor salt-free, thus providing optimal...
<p>The rifting of the Eastern Sardinian margin is considered to have occurred during Neogene, by back-arc extension related eastward migration Apennine subduction system, leading development Tyrrhenian Basin, Western Mediterranean Sea. The locus interpreted first in East-Sardinia Basin (proximal margin), and then Cornaglia Terrace (distal margin). However, dynamics still largely undated, kinematics different domains remains poorly understood. This due sparsity dated rock...
<p>Corrugated detachments are fundamental crustal structures found in many extensional systems and plate tectonic boundaries, including mid-oceanic ridges rifted margins. Direct observations of the complete geometry rare our understanding detachment fault mechanisms development high-angle normal faults their rotation to lower angles mainly relies on proxy observations, for example seismicity trends, numerical modelling.</p><p>We present...
Earth and Space Science Open Archive This preprint has been submitted to is under consideration at Journal of Geophysical Research - Solid Earth. ESSOAr a venue for early communication or feedback before peer review. Data may be preliminary.Learn more about preprints preprintOpen AccessYou are viewing an older version [v2]Go new versionInsights into exhumation mantle hydration processes the Deep Galicia margin from 3D high-resolution seismic velocity modelAuthorsBhargavBoddupalliiDTimothy...
Earth and Space Science Open Archive This preprint has been submitted to is under consideration at Journal of Geophysical Research - Solid Earth. ESSOAr a venue for early communication or feedback before peer review. Data may be preliminary.Learn more about preprints preprintOpen AccessYou are viewing the latest version by default [v3]Insights into exhumation mantle hydration processes Deep Galicia margin from 3D high-resolution seismic velocity modelAuthorsBhargavBoddupalliiDTimothy...
<p>The METYSS project (Messinian Event in the Tyrrhenian from Seismic Study) is based on high-resolution seismic data acquired along Eastern Sardinian margin. The main aim to study Messinian Salinity Crisis (MSC) Western Basin, but we also investigated thinning processes of continental crust and timing crustal vertical movements across this backarc domain. Our first results shown that rifting ended before MSC, activity persisted long after end rifting. This has been...
Earth and Space Science Open Archive This preprint has been submitted to is under consideration at Journal of Geophysical Research - Solid Earth. ESSOAr a venue for early communication or feedback before peer review. Data may be preliminary.Learn more about preprints preprintOpen AccessYou are viewing the latest version by default [v1]Insights into exhumation mantle hydration processes Deep Galicia margin from 3D high-resolution seismic velocity modelAuthorsBhargavBoddupalliiDTimothy...