{"title":"大提顿国家公园精密水准阵测量","authors":"A. Sylvester, Robert B. Smith","doi":"10.13001/UWNPSRC.1994.3217","DOIUrl":null,"url":null,"abstract":"The line was surveyed in 1988, 1989, 1991, and 1993 in each case to a standard deviation of a few parts in 10 million (Sylvester et al., 1991; Byrd 1991). Compared to the initial survey in 1988, the 1993 survey revealed that the floor of Jackson Hole between the Snake River and the Teton Range tilted eastward about 12 microradians toward the Snake River, opposite to the sense of tilt in recent geologic time, judging from the southwestward slope of the valley toward the Teton Range front.","PeriodicalId":321051,"journal":{"name":"University of Wyoming National Park Service Research Center Annual Report","volume":"39 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Survey of Precise Leveling Array Grand Teton National Park\",\"authors\":\"A. Sylvester, Robert B. Smith\",\"doi\":\"10.13001/UWNPSRC.1994.3217\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The line was surveyed in 1988, 1989, 1991, and 1993 in each case to a standard deviation of a few parts in 10 million (Sylvester et al., 1991; Byrd 1991). Compared to the initial survey in 1988, the 1993 survey revealed that the floor of Jackson Hole between the Snake River and the Teton Range tilted eastward about 12 microradians toward the Snake River, opposite to the sense of tilt in recent geologic time, judging from the southwestward slope of the valley toward the Teton Range front.\",\"PeriodicalId\":321051,\"journal\":{\"name\":\"University of Wyoming National Park Service Research Center Annual Report\",\"volume\":\"39 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1900-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"University of Wyoming National Park Service Research Center Annual Report\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.13001/UWNPSRC.1994.3217\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"University of Wyoming National Park Service Research Center Annual Report","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.13001/UWNPSRC.1994.3217","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
摘要
1988年、1989年、1991年和1993年分别对这条线进行了调查，每次的标准偏差都是千万分之几(Sylvester et al.， 1991;伯德1991)。与1988年的初步调查相比，1993年的调查显示，在斯内克河和提顿山脉之间的杰克逊霍尔的地面向斯内克河向东倾斜了大约12微度，与最近地质时期的倾斜感觉相反，从山谷的西南斜坡向提顿山脉前缘判断。
Survey of Precise Leveling Array Grand Teton National Park
The line was surveyed in 1988, 1989, 1991, and 1993 in each case to a standard deviation of a few parts in 10 million (Sylvester et al., 1991; Byrd 1991). Compared to the initial survey in 1988, the 1993 survey revealed that the floor of Jackson Hole between the Snake River and the Teton Range tilted eastward about 12 microradians toward the Snake River, opposite to the sense of tilt in recent geologic time, judging from the southwestward slope of the valley toward the Teton Range front.
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