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- W5537952 abstract "The process that a terrestrialgeologist usually uses to classify a rock is analogousto a flow-chart [1]. The top-level classification(igneous, sedimentary, or metamorphic) is made first.Then further subdivisions are made until the properrock name is determined. Further observations maylead to additional descriptors being added to the frontof the rock name. Thus, a rock may be successivelydetermined to be (1) sedimentary, (2) clastic sedi-mentary, and (3) sandstone. While sandstone is aproper classification of the rock, further observationslead to the addition of descriptors so the final classi-fication could be “tan, immature, massive arkosicsandstone.”The division of rocks at the top level has pro-duced fundamental divisions in the geologicalsciences. These fundamental divisions can lead tosituations that must appear bizarre to a non-geologist.For example, a clast >64 mm in diameter is classifiedas a" @default.
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- W5537952 date "2004-03-01" @default.
- W5537952 modified "2023-09-23" @default.
- W5537952 title "Systematic Rock Classification in a Data-poor Environment: Application to Mars" @default.
- W5537952 hasPublicationYear "2004" @default.
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