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Optical characteristics of minerals were described and photographs were taken with petrographic samples.
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The optical characteristics of the minerals are described below and photographs were taken.
A flow-through method for measuring dissolution rates of cement minerals is described.
A general-purpose, on-line, continuous flow method for determination of δD and δ18O values of water and hydrous minerals is described.
In the petrology, the rock-forming minerals are described in descending order, and one thin-section sometimes contain the minor minerals but other times lack them even in the same rock sample.
The origin of development of the technique and the working hypothesis of the mechanism of high voltage electrical pulse liberation of minerals are described, and the state of the contemporary design and construction of pulse generators are discussed.
These minerals are described as 'free' silica as the SiO2 is not attached to another element to create a new mineral.
It is a property by which minerals may be described relative to a standard scale of 10 minerals known as the Mohs scale of hardness.
Traditionally, minerals have been described as resulting exclusively from inorganic processes; however, current mineralogic practice often includes as minerals those compounds that are organically produced but satisfy all other mineral requirements.
At the beginning of the review period Schindler et al. (240) reported a study of vanadium minerals, and subsequently Schindler and Hawthorne(147) published a detailed approach to the analysis of complex minerals which is described in more detail in section 11.
At the mineralogically famous Långban iron and manganese mines in central Sweden, more than 50 species of arsenate minerals have been described, many peculiar to the locality.
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