Abstract The Leipzig-Regensburg fault zone is documented as a band of seismic activity extending northwards from the earthquake swarm region NW-Bohemia/Vogtland at Czech-German border area and intersected by several Hercynian zones. Along zone, there are areas, northernmost which Schöneck Werdau. In this study, we investigate presumably fluid-induced Werdau area. For purpose, apply two methods:...

Purpose. Identification of the nature manifestation tectonic elements different ages in Central Kazakhstan gravitational fields based on results calculation regional, intra-crustal and local transformants. Methodology. Synthesis analysis data integrated interpretation modeling gravitational, geomagnetic, geothermal fields, latest movements Earth’s crust parameters seismic regime, tectonics stra...

As part of the Variscan orogen, Pyrenean realm has undergone several rifting episodes, starting from Permian-Carboniferous post-orogenic collapse and culminating with mid-Cretaceous lithospheric mantle exhumation. We present Pressure-Temperature-time-deformation (P-T-t-d) evolution tonalite bodies (here described for first time) intruded in late Carboniferous high pressure (HP) granulites Salei...

Climate change effects on snow cover and thermic regime in alpine tundra might lead to a longer growing season, but could also increase risks to plants from spring frost events. Alpine snowbeds, i.e. alpine tundra from late snowmelt sites, might be particularly susceptible to such climatic changes. Snowbed communities were grown in large monoliths for two consecutive years, under different mani...

Cover illustration: The cover image is based on the Technical Note A CRISPR/Cas9-engineered mouse carrying a conditional knockout allele for early growth response-1 transcription factor by Vineet K. Maurya et al., https://doi.org/10.1002/dvg.23515.

Improving the recognition of paleo-fluid circulation history is great significance to reconstruct pore evolution during carbonate diagenesis. Integrated petrography, fluid inclusion, isotopic and elemental geochemistry (laser ablation inductively coupled plasma mass spectrometry) studies, calcites generated in paleocaves, fractures were investigated. This study aims reveal origin karstification...

Ice-core records show that climate changes in the past have been large, rapid, and synchronous over broad areas extending into low latitudes, with less variability over historical times. These ice-core records come from high mountain glaciers and the polar regions, including small ice caps and the large ice sheets of Greenland and Antarctica.