GLOSSARY ENTRY (DERIVED FROM QUESTION BELOW) | ||||||
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23:29 Apr 30, 2021 |
Spanish to English translations [PRO] Science - Mining & Minerals / Gems / technical report | |||||||
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| Selected response from: Marcelo Viera Uruguay Local time: 12:05 | ||||||
Grading comment
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Summary of answers provided | ||||
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3 +3 | concordant to the schistosity |
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4 | consistent with mudstone rock/ shale type |
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3 | coinciding with the modified rock shapes |
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Summary of reference entries provided | |||
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Discussion entries: 1 | |
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consistent with mudstone rock/ shale type Explanation: https://en.wikipedia.org/wiki/Schist |
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concordant to the schistosity Explanation: concordant to the schistosity in the adjacent semipelites. The hornblende lies in the foliation and is lineated. https://www.google.com/url?sa=t&rct=j&q=&esrc=s&source=web&c... -------------------------------------------------- Note added at 49 mins (2021-05-01 00:18:33 GMT) -------------------------------------------------- [shis′täs·əd·ē] (geology) A type of cleavage characteristic of metamorphic rocks, notably schists and phyllites, in which the rocks tend to split along parallel planes defined by the distribution and parallel arrangement of platy mineral crystals. https://encyclopedia2.thefreedictionary.com/schistosity -------------------------------------------------- Note added at 1 hr (2021-05-01 00:50:53 GMT) -------------------------------------------------- En geología se denomina esquistosidad a la propiedad de ciertas rocas y suelos, notablemente los esquistos o pizarras, que les lleva a organizarse en láminas o superficies paralelas entre sí. Está ligada a la microestructura del material, pues en ciertas configuraciones la presencia de una fuerza perpendicular permite la reordenación de los minerales que lo forman. https://es.wikipedia.org/wiki/Esquistosidad -------------------------------------------------- Note added at 18 hrs (2021-05-01 18:13:58 GMT) -------------------------------------------------- Schistosity, mode of foliation that occurs in certain metamorphic rocks as a consequence of the parallel alignment of platy and lath-shaped mineral constituents. It reflects a considerable intensity of metamorphism—i.e., changes resulting from high temperatures, pressures, and deformation. https://www.britannica.com/science/schistosity |
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