Results 121 to 130 of about 17,606 (188)

Explainable machine learning framework for assessing groundwater quality and trace element contamination in Eastern Saudi Arabia. [PDF]

Sci Rep
Aldrees A, Jibrin AM, Dan'azumi S, Mahmoud IA, Aliyu UU, Abba SI.   +5 more
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Paleoproterozoic Mississippi Valley-type mineralization at Black Angel, Greenland: evidence from sulfide δ⁶⁶Zn and rhenium-osmium geochronology. [PDF]

Miner Depos
Saintilan NJ, Archer C, Szilas K, Krüger Geertsen K, Rosa D, Spangenberg JE.   +5 more
europepmc   +1 more source

Revisiting the Eoarchean Akilia quartz-pyroxene rock with potassium isotopes: Implications for early-ocean sedimentation. [PDF]

Proc Natl Acad Sci U S A
Long ZY, Moynier F, Dai W, van Zuilen M, Deng J, Qiu KF.   +5 more
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A dataset and benchmark of carbonate thin-section images for deep learning. [PDF]

Sci Data
Li K, Song J, Zhang Z, Ren S, Lan Y, Yang D, Li Z, Liu S, Yan C, Jin X, Yang S, Guo J.   +11 more
europepmc   +1 more source

Global dataset of nearshore and submarine springs. [PDF]

Data Brief
Bouimouass H, Fourno A, Hamon Y, Chalikakis K.   +3 more
europepmc   +1 more source

Groundwater nitrate response to hydrogeological conditions and socioeconomic load in an agriculture dominated area. [PDF]

Sci Rep
Jia H, Qian H.
europepmc   +1 more source

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Evaporite minerals succession

Crystal Research and Technology, 1987
AbstractAn explanation is given for the crystallization succession during sea‐water evaporation, namely for the differences between the equilibrium solubility diagram of the marine‐type system and the “solar diagram”: The magnesium ions are known to exist in sea‐type solutions predominantly as hexaaqua complexes.
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Engineering properties of evaporites and evaporitic formations of Turkey

Bulletin of the International Association of Engineering Geology, 1982
Although the known evaporite minerals amount to more than 25, anhydrite and gypsum are the most conspicuous from the engineering geological point of view. They present considerable difficulties in the construction of tunnels, dams and other structures because of their solubility and swelling when treated with water.
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EVAPORITES : A SYMPOSIUM

Proceedings of the Yorkshire Geological Society, 1948
(Read, September, 1947, at a Joint General Meeting with the Teeside Section of the Royal Institute of Chemistry). EVAPORITES BY S. E. HOLLINGWORTH I should like first of all to express my pleasure that the subject of “Evaporites” has been chosen for this joint discussion and also to thank you for asking me to take part. Rocks formed by precipitation
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Deposition of Evaporites

AAPG Bulletin, 1953
Modern oceanographic studies in estuaries and other restricted arms of the sea have shown that a characteristic circulation pattern exists. Surface currents flow from regions of low salinity to regions of higher salinity in response to hydrostatic head and are accompanied at depth by oppositely directed currents flowing from high to low salinity ...
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