Results 181 to 190 of about 12,827 (272)
Abstract Capillary pressure‐saturation relationships are crucial for geo‐energy recovery, and increasingly, for environmental applications. However, for reservoir‐relevant pressure and temperature conditions, only limited data sets are available from special core analysis in laboratory (SCAL) studies.
Juliane Kummerow +2 more
wiley +1 more source
Recurrent and Long-Term Oceanic Anoxia Contributed to Aborted Biotic Recovery Following the Permian-Triassic Crisis. [PDF]
Li W, Yuan B.
europepmc +1 more source
The Origin of Carbonate Magmas Predating and Accompanying Main‐Phase LIPs Eruptions
Abstract Some large igneous provinces (LIPs) are associated with precursory carbonatite eruptions. Models for precursory carbonatites invoking partial melting of a carbonate metasomatized lithosphere appear implausible, given the long time needed for heat conduction from the plume head.
Cinzia G. Farnetani, Mark A. Richards
wiley +1 more source
Pulsed volcanic sulfur emissions linked to the end-Triassic terrestrial crisis. [PDF]
Fang L +16 more
europepmc +1 more source
A small short-necked hupehsuchian from the lower Triassic of Hubei Province, China. [PDF]
Chen XH +4 more
europepmc +1 more source
Abstract We estimate the cosmic dust flux to Earth through the study of rare micrometeorites that preserve part of their precursor features during atmospheric entry heating, namely unmelted and scoriaceous subtypes. Combining high‐precision mass balance measurements, X‐ray computed microtomography and scanning electron microscopy, we studied mass, size
S. Ottaviani +7 more
wiley +1 more source
Revisiting the enigmatic Cheirolepidiaceae: origins, phylogenetic relationships, and a new whole-plant concept. [PDF]
Andruchow-Colombo A, Matsunaga KKS.
europepmc +1 more source
Abstract The Gaggiano High, buried beneath the sediments of the Western Po Plain (northern Italy), represents one of the few examples of Mesozoic structural highs largely preserved within a foreland–foredeep system. Unlike the adjacent Lacchiarella Basin, which underwent strong positive inversion during the Neogene, the Gaggiano High experienced only ...
M. Mercuri +7 more
wiley +1 more source
The Megalopolis Basin is located in the central Peloponnese (Greece), a region that is situated along one of the primary Pleistocene biogeographical corridors for intracontinental hominin migration. The basin comprises several hundred metres of Plio‐Pleistocene sediments alternating between clastics and lignites.
Ines J. E. Bludau +13 more
wiley +1 more source
Non‐Uniqueness, Symmetries and Invariance of Thermal History Modelling in Sedimentary Basins
This paper approaches non‐unique inverse problems by generating a representative ensemble of all possible solutions using the concept of symmetry. In the context of basin modelling, a symmetry is any manipulation of a forward model's parameters (e.g., thermal history) that leaves the model output (e.g., downhole vitrinite reflectance) unchanged ...
J. Xiao, D. Waltham, Y. Wang
wiley +1 more source

