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- W2084067961 abstract "ABSTRACT Certain Miocene units in the southeastern Caliente Range of California contain polished pebbles. The polished surfaces of these pebbles are crossed by parallel microstriations, tiny polished grooves similar in appearance to slickenside striae. Within a single bed or sequence of beds, the striations have a pronounced overall orientation approximately normal to the regional structural trend. This alignment precludes a predepositional origin for the polish and suggests that internal movement during deformation polished the pebbles. Parallel microstriations also occur on polished pebbles from various units elsewhere, suggesting that tectonic polish may be fairly common." @default.
- W2084067961 created "2016-06-24" @default.
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- W2084067961 date "1965-01-01" @default.
- W2084067961 modified "2023-09-25" @default.
- W2084067961 title "Tectonic Polish of Pebbles" @default.
- W2084067961 doi "https://doi.org/10.1306/74d71389-2b21-11d7-8648000102c1865d" @default.
- W2084067961 hasPublicationYear "1965" @default.
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