Results 191 to 200 of about 402,108 (304)
Region-specific LOI-TOC conversion models for marine sediment blue carbon assessment in the Western Irish Sea. [PDF]
Grey A +6 more
europepmc +1 more source
Revista Muzeul Mineralogic-Geologic al Universităţii din Cluj la Timişoara
Muzeu Mineralogic-Geologic
core
Formed ~1.4 Ga, the carbonate reservoir of the Jixian System is a key geothermal reservoir in northern China. Differential basin–mountain evolution since the Cenozoic led to distinct reservoir‐forming histories; consequently, this same reservoir shows marked productivity contrasts between intramontane basins and the large rift Bohai Bay Basin ...
Chuanqing Zhu +6 more
wiley +1 more source
Tectonism rather than "snowball Earth" glaciation is responsible for the Great Unconformity. [PDF]
Zhan RR +11 more
europepmc +1 more source
1. The synergistic effects of carbonate mineral dissolution, coal matrix drying/shrinkage, and supercritical CO2 (ScCO2)‐induced organic matter extraction collectively enhance pore/fracture connectivity, thereby significantly improving permeability. 2.
Junwen Zhou, Enguang Han
wiley +1 more source
Effects of dichlofluanid in tropical marine bivalves exposed to water and spiked sediments: an assessment of biomarker responses. [PDF]
Cruz ACF +6 more
europepmc +1 more source
Abstract Efforts to use transcriptomics for toxicity testing have classically relied on the assumption that chemicals consistently produce characteristic transcriptomic signatures that are reflective of their mechanism of action. However, the degree to which transcriptomic responses are conserved across different test methodologies has seldom been ...
Paul Béziers +10 more
wiley +1 more source
Feedback Between Climate and Geodynamics Leads to Bistability in Conceptual Models
Görg K, Eberhard J, Feulner G.
europepmc +1 more source
A GIS-based AHP approach integrating geospatial and magnetic data for groundwater potential mapping in a structurally complex arid region, Egypt. [PDF]
Zamzam S +3 more
europepmc +1 more source
Coupled dissolution‐reprecipitation of early formed Cd‐, Fe‐, Ag‐ and Sb‐poor sphalerite through interaction with high‐temperature and high‐sulphur fugacity Cu‐rich fluids, responsible for the formation of the yellow ores, resulted in the formation of Cd‐, Fe‐, Ag‐ and Sb‐rich, heavily chalcopyrite‐diseased sphalerite and enrichment of critical metals ...
Manuel Nopeia +4 more
wiley +1 more source

