Results 71 to 80 of about 20,638 (213)

Magnetic Fabrics and Petrography of Rocksalts Reveal Preferred Orientation of Anhydrites Within a Halite Matrix

open access: yes, 2022
The ecxel file contain the magnetic data used in: Issachar, R.; Weinberger, R.; Levi, T.; Barabasch, J.; Urai, J.L. Magnetic Fabrics and Petrography of Rocksalts Reveal Preferred Orientation of Anhydrites Within a Halite Matrix.
ran issachar (4623076)
core   +1 more source

Lithogenesis on peneplaned сontinented platform of Kazakhstan and Siberia during the Cretaceous-Paleogene boundary epoch

open access: yesЛитосфера, 2019
Research subject. The inner structure, composition, and genesis of the poorly studied formation of weathering crusts are studied with reference to peneplaned platform territories in Kazakhstan and Siberia during the Cretaceous-Paleogene boundary epoch ...
Yu. G. Tsekhovskii   +2 more
doaj   +1 more source

Geochemical and granulometric fingerprints of 8200 years of westerly wind variability in inner‐fjord lake sediments from Svalbard

open access: yesBoreas, EarlyView.
The Arctic is warming faster than any other region on Earth. As sea ice diminishes, the surface boundary conditions, such as roughness and air–sea coupling, change and open‐water fetch increases. This may enhance wind forcing on Arctic coasts. Lake sediments can record these changes through the deposition of wind‐blown grains and elements, offering ...
Zofia Stachowska   +5 more
wiley   +1 more source

Automated petrography applications in Quaternary Science

open access: yes, 2011
Automated petrography analysis integrates scanning electron microscopy and energy-dispersive x-ray spectroscopy (SEM-EDS) hardware with expert software to generate micron-scale compositional maps of rocks and sediments.
Haberlah, David   +6 more
core  

(Table 1) Petrography of Fe-Ti oxide gabbros from ODP Hole 118-735B

open access: yes, 1991
(Table 1) Petrography of Fe-Ti oxide gabbros from ODP Hole 118 ...
Peter S Meyer (6963035)   +5 more
core   +1 more source

Thortveitite-type Tm2Si2O7

open access: yesActa Crystallographica Section E, 2014
Single crystals of dithulium disilicate, Tm2Si2O7, were obtained in flux synthesis experiments in the system SiO2–Tm2O3–LiF at ambient pressure. The compound belongs to the group of sorosilicates, i.e. it is based on [Si2O7]-units and crystallizes in the
Volker Kahlenberg, Paul Aichholzer
doaj   +1 more source

Quantitative methods for quantification of montmorillonite content in bentonite clays

open access: yesGeoresursy, 2020
This article is devoted to the comparison of various methods for the quantitative determination of montmorillonite content in bentonite clays based on the adsorption of organic molecules and cations.
Petr E. Belousov   +3 more
doaj   +1 more source

Appraisal of Six Natural Mica Reference Materials for In Situ Rb‐Sr Geochronology

open access: yesGeostandards and Geoanalytical Research, EarlyView.
Key Points Evaluated six natural mica reference materials for in situ LA‐ICP‐MS/MS Rb‐Sr geochronology using geochemical, microstructural and isotopic characterisation. Identified robust primary reference materials: Mount Dromedary biotite (99.37 Ma) and Mica‐Fe biotite (307.75 Ma). La Posta biotite and Högsbo muscovite are suitable secondary reference
Hugo K.H. Olierook   +38 more
wiley   +1 more source

(Table 2) Petrography of volcaniclastic sandstones from Unit III of ODP Hole 135-840B

open access: yes, 1994
(Table 2) Petrography of volcaniclastic sandstones from Unit III of ODP Hole 135 ...
Bøe, Reidulv, Reidulv Bøe (4317967)
core   +1 more source

The Role of Placer Deposits in Ensuring the Reproduction of the Mineral Resource Base of Scarce Types of Strategic Mineral Raw Materials in Russia at the Present Stage

open access: yesRussian Journal of Earth Sciences
Placer deposits had (and for a number of components still have) an important role in providing strategic types of mineral resource base for both Russia and the world as a whole.
Bortnikov N. S.   +5 more
doaj   +1 more source

Home - About - Disclaimer - Privacy