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CAMSIZER Particle Size Data from Explosive Paroxysms of Mt. Etna (2011–2025)

Mt. Etna in Catania, Italy, is an active volcano that has served as a natural laboratory for many volcanologists worldwide. Its paroxysms are unique eruptive events caused by a complex magmatic system that, despite being one of the most studied volcanoes, there is still an open field to contribute to the understanding of magma dynamics and degassing. This data set is a compilation of grain-size and shape measurements of 14 tephra samples of Mt. Etna. The tephra samples correspond to some of the most explosive cycles and events of the volcano from 2011 to 2025. The measurements were obtained using CAMSIZER through the ILGE TNA grant funding at INGV sezione di Catania. This dataset is the basis for a research project investigating the controls on the volume of gases and magma emitted during an eruption of Mt. Etna. This publication results from work conducted under the transnational access/national open access action at Sedimentology Laboratory – INGV sezione di Catania supported by WP3 ILGE - MEET project, PNRR - EU Next Generation Europe program, MUR grant number D53C22001400005.

Rheology of PDMS Korasilon G20OH (#1000039264) used at the Laboratory for Experimental Tectonics at GFZ Helmholtz Centre for Geosciences, Potsdam, Germany

This dataset provides rheometric data of the PDMS Korasilon G 20 OH used for analogue modelling at the Laboratory for Experimental Tectonics at GFZ Helmholtz Centre for Geosciences, Potsdam, Germany. The batch number is 1000039264, purchased in 2022 and opened in 2026. The material sample has been analyzed at the Laboratory for Experimental Tectonics at GFZ Helmholtz Centre for Geosciences, Potsdam (HelTec) using an Anton Paar Physica MCR 301 rheometer in a cone-plate configuration at room temperature (21˚C). Rotational (controlled shear rate) tests with shear rates varying from 10^-4 to 10^-1 s^-1 were performed. According to our rheometric analysis, the material is quasi-Newtonian (n~1) at strain rates below 10^-2 s^-1 and weakly shear rate thinning above. The viscosity of G 20 OH is 1.8*10^4 Pa s.

Crystal Size Distribution Analyses of Isothermal Deformation Experiments

In this work we aimed to investigate and quantify the relative importance of dynamic conditions (e.g., stirring in a Concentric Cylinder apparatus) on the crystallization kinetics of basaltic magmas (Stromboli). This was achieved by observing the final textures of the samples, analysing the resulting SEM images, and finally relating the resulting parameters to specific growth and nucleation rates. The dataset is made of: 1) A folder called "SEM Images" with two sub-folders inside, representative of the two experiments carried out, called "CG1" and "CG2.3" 2) An Excel file, consisting in 4 data sheets, where all results of image analysis are included, divided in sections. The sheets are also available in CSV format. This publication results from work conducted under the transnational access/national open access action at High Pressure - High Temperature Laboratory (HPHT Lab), Istituto Nazionale di Geofisica e Vulcanologia (INGV), Rome, Italy supported by WP3 ILGE - MEET project, PNRR - EU Next Generation Europe program, MUR grant number D53C22001400005.

Neuartige Porosierungsmittel aus der hydrothermalen Behandlung feuchter biogener Reststoffe, insbesondere Klärschlamm, KMU-innovativ -KMUi-BÖ07: Resi2Pores - Neuartige Porosierungsmittel aus der hydrothermalen Behandlung feuchter biogener Reststoffe, insbesondere Klärschlamm

Dataset of wehrlitization process: insights from X-ray Micro-CT of Mt. Vulture (southern Italy) mantle xenoliths

The study of textural and chemical characteristics of mafic minerals from mantle xenoliths is essential to investigate the nature of the upper mantle in a continental geodynamic context, melts generation and their effects related to mantle metasomatism. Particular textures in mantle minerals, inclusions or secondary veins of different nature (silicates vs carbonates), bubbles, represent petrographic tools to investigate these processes within the mantle. Petrographic 2D thin sections might overlook these mineralogical features, and 3D textural analysis through X-ray computed microtomography (micro-CT) are crucial to overcome these limitations. We focused on the Mt. Vulture volcano (southern Italy) rare mantle xenoliths, brought to the surface by a melilitite-carbonatite magma (141 ka), with particular emphasis to spinel-wehrlite xenoliths and wehrlitization processes that is located close to an area of intense CO2 degassing associated to catastrophic earthquakes. Preliminary results showed interesting 3D textural distributions within the studied xenoliths-forming mantle minerals. In particular, the micro-CT allowed to furnish new constrains on the relationship between fluids entrapment and migration, and structural discontinuities. Indeed, some minerals (especially those from the wehrlite xenoliths) showed a well-correlated distribution of fluid inclusions along the secondary fracturing planes. This publication results from work conducted under the transnational access/national open access action at Istituto Nazionale di Geofisica e Vulcanologia – Osservatorio Vesuviano (INGV-OV) and supported by WP3 ILGE - MEET project, PNRR - EU Next Generation Europe program, MUR grant number D53C22001400005. The author thanks also Gianmarco Buono and Lucia Pappalardo for their support during the analyses and the post processing process.

Naturschutzgebiete nach Aktionsplan Ostseeschutz 2030

Die Gebietsabgrenzungen der Naturschutzgebiete (NSG) im Aktionsplan Ostseeschutz 2030 gemäß der Verordnungen vom 11.03.2026 werden umgehend in den Gesamt-Datenbestand der Naturschutzgebiete aufgenommen. Bis dahin ist eine kartografische Darstellung nicht möglich. Der Download der Daten ist hier möglich. Die Abgrenzungen sind die linienhaften Verbindungen zwischen den Stützpunkten gemäß der Verordnungen.

Untersuchungen der energetischen Nutzungsoptionen von Hanffaserreststoffen zur exemplarischen Einbindung in das Energiekonzept eines Verarbeitungsstandorts

Die Hanfindustrie hat sich in den vergangenen Jahren aufgrund neuer politischer Rahmenbedingungen und innovativer Produktfelder zu einem stark wachsenden Wirtschaftsbereich entwickelt. Hanfprodukte werden in der Lebensmittel-, Pharma-, Automobil-, Bau-, Textil- und Papierindustrie eingesetzt. Das stärkste Wachstum der Hanfindustrie findet in der Produktion von Lebensmittel- und Lebensmittelzusätzen aus Hanfsamen, Hanf- und CBD-Ölen statt. Als Nebenprodukte fallen in diesen Wirtschaftsbereichen Extraktionsreste an, für die es derzeit nur bedingt Verwertungsmöglichkeiten gibt. In der industriellen Hanffaserproduktion werden aus getrocknetem Hanfstroh hochwertige Naturfasern gewonnen, die z.B. im Fahrzeugleichtbau zur Herstellung von Fahrzeugarmaturen und Verkleidungen eingesetzt werden. Hanffasern sind darüber hinaus ein etabliertes ökologisches Dämmstoffmaterial. Hanfdämmstoffe zeichnen sich durch eine bessere CO2 Bilanz gegenüber konventionellen Dämmstoffmaterialien wie Mineralwolle oder Styropor aus und bieten die Möglichkeit CO2 über mehrere Jahrzehnte im Dämmstoff zu fixieren. Im Dämmstoffherstellungsverfahren fallen neben dem Hauptprodukt Hanffasern im etwa gleichen Umfang zellulosehaltige Reststoffe an, die derzeit nur zu einem geringen Teil wirtschaftlich genutzt werden. Im Hinblick auf eine zunehmende regenerative Energieversorgung sowie knapper werdende Ressourcen bzw. der kritischen Diskussion um den Einsatz nachwachsender Rohstoffe zur Energiegewinnung kommt der Erschließung biogener Rest- und Abfallstoffe für die Erzeugung effizienter, speicherbarer, flexibler und dezentraler Bioenergieträger zunehmende Bedeutung zu. Im Vorhaben HanfNRG sollen energetischen Nutzungsoptionen von Reststoffen der Hanfverarbeitung untersucht werden zur exemplarischen Einbindung in das Energiekonzept einer Hanffaserfabrik.

Ring-shear test data of quartz sand SIBELCO S80 used for analogue modelling in the Tectonic Laboratory (TecLab) at Utrecht University

This dataset provides friction data from ring-shear tests on quartz sand SIBELCO S80 used in analogue modelling of tectonic processes as a rock analogue for the earth’s upper crust (e.g., Klinkmüller et al., 2016). According to our analysis the material shows a Mohr-Coulomb behaviour characterized by a linear failure envelope. Peak, dynamic and reactivation friction coefficients of quartz sand S80 are µP = 0.75, µD = 0.59, and µR = 0.69, respectively (Table 5). Cohesion of the material ranges between 0-80 Pa. The material shows no rate-dependency (<1% per ten-fold change in shear velocity v). The tested bulk material consists of quartz sand SIBELCO S80 with grain size of ~0.63-355 µm (D50 = 175 µm. Bulk and grain densities are 1300 kg/m³ and 2650 kg/m³, respectively and the hardness is 7 on Moh’s scale. S80 is sold e.g., by the company SIBELCO (sibelco.com).

Digital Image Correlation data from experiments of releasing bend evolution within different strength wet kaolin

The data set includes the Digital Image Correlation (DIC) results for four experiments of releasing bends along dextral strike-slip faults that were performed at the University of Massachusetts at Amherst (USA). Gabriel et al. (in prep.) used the DIC data sets to investigate how releasing bend fault systems evolve within different strength wet kaolin. Information on the experimental set up and methods can be found in the main text and supplement to Gabriel et al. (in prep.). The data here include the incremental displacement time series, strain animation and surface elevation data at the end of the two experiments with different clay strength, which are presented within Gabriel et al. (in prep). We also include in this data repository incremental displacement time series and strain animations from two experiments that repeat the conditions of the experiments featured in Gabriel et al. (2025).

Results of analogue tectonic models of rifting and tectonic lineament reactivation along the Main Ethiopian Rift

This data set includes results from a total of 13 analogue tectonic models aimed at simulating the activation of tectonic lineaments associated with the Main Ethiopian Rift in eastern Africa. We use a model set-up based on previous work by Zwaan et al. (2021, 2022). This set-up involves a velocity discontinuity (VD, i.e., the edge of a mobile base plate) to induce extension in the overlying brittle- and viscous model materials representing the upper and lower crust, respectively. Additional structural weaknesses (seeds) at the base of the brittle layer serve to represent activated tectonic weaknesses in nature. Model parameters (different VD and seed orientation, and different seed diameters) are summarized in Table 1. The model results presented in this data publication are obtained through Digital Image Correlation (DIC) and Structure-from-Motion (SfM) analyses. A more detailed description of model set-up, model results, and their interpretation can be found in Zwaan et al. (2025)

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