ideas regarding the physical state of the earth's interior; these ideas_ are based on extrapolation from physical constants obtained in the laboratory, and their variety extends to the number of possible permutations and combinations of the three physical states of matter-solid, liquid, and gaseous...
Reconciling magma–ocean crystallization models with the present-day structure of the Earth’s mantle. Geochem. Geophys. Geosyst. 18, 2785–2806 (2017). Article Google Scholar Li, M., McNamara, A. K. & Garnero, E. J. Chemical complexity of hotspots caused by cycling oceanic crust ...
Kuskov, O.L., Kronrod, E.V., Matsumoto, K.et al.Is a Consensus Possible between Geochemical and Geophysical Models of the Internal Structure of the Lunar Mantle?.
Models of the internal structure of Callisto were constructed and the extent of its differentiation was determined based on geophysical information from the Galileo spacecraft (the mass, the radius, the mean density, and the moment of inertia), geochemical data (the chemical composition of meteorite...
The factor structure of the General Health Questionnaire (GHQ): a scaled version for general practice in Spain Eur. Psychiatry, 21 (2006), pp. 478-486, 10.1016/j.eurpsy.2006.03.002 View PDFView articleView in ScopusGoogle Scholar Musterd et al., 2012 S. Musterd, G. Galster, R. Anderss...
François Gerlotto, Jorge ParamoThe three-dimensional morphology and internal structure of clupeid schools as observed using vertical scanning multibeam sonar Aquatic Living Resources, 16 , 113 -122 (2003) S. Mathis, N. de BryeLow-frequency internal waves in magnetized rotating stellar radiation zo...
PDF Tools Share Abstract The Pacific Ocean, spanning over 30% of the Earth's surface, provides an ideal setting for studying the surface radiative balance due to its relatively pristine atmospheric conditions, far from anthropogenic emission sources. In this study we investigated the causes for the...
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However, the internal structure of a lava dome, particularly the extent of the surrounding low-density talus has been an unknown factor although it is likely critical to prediction of its collapse magnitude1. The lava dome generally consists of two units: a relatively soft interior (core) and ...
small areas or low-resolution imagery on larger areas. This makes it difficult to assess a three dimensional and detailed view of the volcano internal structure. Figure 1 Presentation of the most active part ofPiton de la Fournaise: theEnclos Fouquécaldera. (A) skyTEM device over thePiton de...