Spatial distribution patterns and causal mechanisms of rainfall-induced clustered landslides: A case study from Southwestern Yunnan Province, China. [PDF]
Xu Z, Zeng Y, Li Y, Yang M.
europepmc +1 more source
Abstract Historical biogeography faces a persistent conceptual and methodological dilemma concerning the nature of its central analytical units. Using the recent proposal by Schultz and Cracraft (Cladistics 40, 653) as a catalyst, this article critiques the argument that causal inference necessitates the replacement of areas of endemism with barriers ...
Augusto Ferrari
wiley +1 more source
Insights into the seismogenesis and tectonic implications of an isolated intraplate earthquake (M4.0) on February 17, 2025, in Delhi. [PDF]
Prajapati SK +4 more
europepmc +1 more source
Controls on hydrocarbon accumulation in ultra-deep carbonate reservoirs of the Ordovician Yingshan Formation, Catake Uplift, Tarim Basin. [PDF]
Wang L +5 more
europepmc +1 more source
Deciphering grain-size reduction as a driver of mid-lithosphere discontinuity formation. [PDF]
Liu M +4 more
europepmc +1 more source
Structural barriers control the spatial extent of slow earthquake slip. [PDF]
Akuhara T +18 more
europepmc +1 more source
Integrated multi-scale aeromagnetic, gravity, and remote-sensing analysis for mapping basement fabric and structural architecture in the ِِِAswan region, Southern Egypt. [PDF]
Khalifa M +6 more
europepmc +1 more source
Stress variability and brittle tectonic structures
The problem of stress variability, both in space and time, during brittle deformation of rocks is faced in this note. Several possible causes of the temporal and spatial variations of the stress tensor are reviewed and discussed. A genetic partitioning of the stress tensor is proposed, showing that any stress field within a crustal volume can be seen ...
CAPUTO, Riccardo
openaire +2 more sources
End Late Paleozoic tectonic stress field in the southern edge of Junggar Basin
This paper presents the end Late Paleozoic tectonic stress field in the southern edge of Junggar Basin by interpreting stress-response structures (dykes, folds, faults with slickenside and conjugate joints).
Wei Ju
exaly +2 more sources

