1982 . Density of minerals and rocks under shock compression . In Landolt-Börnstein—Numerical data and functional relationships in science and technology , edited by Angenheister G. Berlin: Springer. pp. 120 – 183 .Stoffler D. 1982. Density of minerals and rocks under shock compression. ...
3.Rock density structure in Bangong-Nujiang suture zone and its significance青藏高原班公湖-怒江缝合带域岩石密度结构及意义 4.Development of Low-Power Intelligence Density Meter for Measuring Rocks and Minerals低功耗智能岩(矿)石密度测定仪的研制 5.The acoustic velocity of a rock varies according to...
2) densities of rocks and minerals 岩矿石密度3) rock and mineral density 岩(矿)石密度 例句>> 4) compact ore 致密矿石5) mineral content density 含矿密度 1. Based on theory of ore forming,the concept of mineral content density is first established. 从成矿理论出发 ,先提出含矿密度...
Densities of Rocks and Minerals. In Practical Handbook of Physical Properties of Rocks and Minerals; Carmichael, R.S., Ed.; Section II; CRC Press: Boca Raton, FL, USA, 1989; pp. 1–38. [Google Scholar] Publisher’s Note: MDPI stays neutral with regard to jurisdictional claims in ...
Therefore, bulk density has a strong correlation with minerals, fluids, and porosity, which can be obtained from the following equation: (2.1)ρb=1−ϕρm+ϕρf where ρb is the bulk density of the rock; ρm is the matrix or mineral density; ϕ is the porosity of the rock; ...
Mineral density, or the mass per volume, and specific gravity, or the ratio of mass to an equal volume of water, are used to identify minerals...
(VCM) are derived through the use of the VP(z), VS(z) seismic velocity models, petrological data, measurements of VP, VS, density (rho) and mean atomic weight (m) for several groups of rocks and minerals of different composition and genesis, as well as from pressure and temperature ...
Ch 3. Characteristics of Matter Ch 4. Earth's Spheres and Internal... Ch 5. Plate Tectonics Ch 6. Minerals and Rocks Ch 7. Igneous Rocks Ch 8. Volcanic Landforms Ch 9. Weathering and Erosion Ch 10. Sedimentary Rocks: A Deeper Look Ch 11. Metamorphic Rocks: A Deeper Look Ch 12. Ro...
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By using the principal thermal expansions and compressibilities of individual minerals, and simplifying assumptions, we are able to predict crack densities as a model rock is subjected to changes of P and T. Experimental crack densities for three granitic rocks, a gabbro, and two basalts are ...