Ultramicroscopie petrographique; le rutile du quartz des granites
1964 ◽
Vol S7-VI
(2)
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pp. 181-187
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Abstract Rutile needles of macroscopic, microscopic, and submicroscopic sizes occur in the quartz of acidic igneous rocks. Although it is not known whether they are present as the result of mechanical inclusion, crystallization simultaneous with that of the quartz, oriented exsolution, or replacement they are an important means of tectonic and geochemical study. A grain of granitic quartz torn by erosion from its crystalline petrographic context retains its submicroscopic inclusions throughout the course of its sedimentary peregrinations no matter how small the detrital fragments may become.
2000 ◽
Vol 139
(4)
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pp. 436-457
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2020 ◽
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2020 ◽
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2020 ◽
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1983 ◽
Vol 47
(342)
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pp. 1-9
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