Rate of change of the Quincy-Monument Peak baseline from a translocation analysis of LAGEOS Laser Range Data
Translocation studies of Lageos laser range data from Quincy and Monument Peak in California observed during 1984-1987 suggest that plate tectonic motion across the San Andreas fault system in the direction of the baseline between the two stations is uniform at a rate of -30(+ or - 3) mm/yr. Changes...
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| Veröffentlicht in: | Geophysical research letters 1989-06, Vol.16 (6), p.539-542 |
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| container_title | Geophysical research letters |
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| creator | Stolz, A. Vincent, M. A. Bender, P. L. Eanes, R. J. Watkins, M. M. Tapley, B. D. |
| description | Translocation studies of Lageos laser range data from Quincy and Monument Peak in California observed during 1984-1987 suggest that plate tectonic motion across the San Andreas fault system in the direction of the baseline between the two stations is uniform at a rate of -30(+ or - 3) mm/yr. Changes in the components of the baseline vector were inferred from repeat determinations using the solutions from successive 0.5-year intervals. The changes in the vertical and transverse components of the Quincy-Monument Peak baseline are -0.4(+ or - 5) mm/yr and +14(+ or -5) mm/yr, respectively. The vertical component determinations attest to the height stability of the laser ranging method. Lageos measurements made from Quincy and Monument Peak before 1984 are inaccurate enough to limit their usefulness for plate tectonic studies. |
| doi_str_mv | 10.1029/GL016i006p00539 |
| format | Article |
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A. ; Bender, P. L. ; Eanes, R. J. ; Watkins, M. M. ; Tapley, B. D.</creator><creatorcontrib>Stolz, A. ; Vincent, M. A. ; Bender, P. L. ; Eanes, R. J. ; Watkins, M. M. ; Tapley, B. D.</creatorcontrib><description>Translocation studies of Lageos laser range data from Quincy and Monument Peak in California observed during 1984-1987 suggest that plate tectonic motion across the San Andreas fault system in the direction of the baseline between the two stations is uniform at a rate of -30(+ or - 3) mm/yr. Changes in the components of the baseline vector were inferred from repeat determinations using the solutions from successive 0.5-year intervals. The changes in the vertical and transverse components of the Quincy-Monument Peak baseline are -0.4(+ or - 5) mm/yr and +14(+ or -5) mm/yr, respectively. The vertical component determinations attest to the height stability of the laser ranging method. Lageos measurements made from Quincy and Monument Peak before 1984 are inaccurate enough to limit their usefulness for plate tectonic studies.</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/GL016i006p00539</identifier><language>eng</language><publisher>Legacy CDMS: Blackwell Publishing Ltd</publisher><subject>580000 - Geosciences ; ACCURACY ; CALIFORNIA ; DEVELOPED COUNTRIES ; FEDERAL REGION IX ; GEOLOGIC FAULTS ; GEOLOGIC FRACTURES ; GEOLOGIC STRUCTURES ; Geophysics ; GEOSCIENCES ; Intervals ; LASERS ; Mathematical analysis ; MONITORING ; NORTH AMERICA ; PLATE TECTONICS ; REMOTE SENSING ; SATELLITES ; Stability ; Stations ; STRATA MOVEMENT ; TECTONICS ; USA ; Vectors (mathematics)</subject><ispartof>Geophysical research letters, 1989-06, Vol.16 (6), p.539-542</ispartof><rights>Copyright 1989 by the American Geophysical Union.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a4579-9460e79cdfb3d81e1021f4ff8fbeb13166417a9fbf719a975567c9aa619a5a393</citedby><cites>FETCH-LOGICAL-a4579-9460e79cdfb3d81e1021f4ff8fbeb13166417a9fbf719a975567c9aa619a5a393</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2FGL016i006p00539$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2FGL016i006p00539$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>230,314,776,780,881,1411,27901,27902,45550,45551</link.rule.ids><backlink>$$Uhttps://www.osti.gov/biblio/5599253$$D View this record in Osti.gov$$Hfree_for_read</backlink></links><search><creatorcontrib>Stolz, A.</creatorcontrib><creatorcontrib>Vincent, M. A.</creatorcontrib><creatorcontrib>Bender, P. L.</creatorcontrib><creatorcontrib>Eanes, R. J.</creatorcontrib><creatorcontrib>Watkins, M. M.</creatorcontrib><creatorcontrib>Tapley, B. D.</creatorcontrib><title>Rate of change of the Quincy-Monument Peak baseline from a translocation analysis of LAGEOS Laser Range Data</title><title>Geophysical research letters</title><addtitle>Geophys. Res. Lett</addtitle><description>Translocation studies of Lageos laser range data from Quincy and Monument Peak in California observed during 1984-1987 suggest that plate tectonic motion across the San Andreas fault system in the direction of the baseline between the two stations is uniform at a rate of -30(+ or - 3) mm/yr. Changes in the components of the baseline vector were inferred from repeat determinations using the solutions from successive 0.5-year intervals. The changes in the vertical and transverse components of the Quincy-Monument Peak baseline are -0.4(+ or - 5) mm/yr and +14(+ or -5) mm/yr, respectively. The vertical component determinations attest to the height stability of the laser ranging method. Lageos measurements made from Quincy and Monument Peak before 1984 are inaccurate enough to limit their usefulness for plate tectonic studies.</description><subject>580000 - Geosciences</subject><subject>ACCURACY</subject><subject>CALIFORNIA</subject><subject>DEVELOPED COUNTRIES</subject><subject>FEDERAL REGION IX</subject><subject>GEOLOGIC FAULTS</subject><subject>GEOLOGIC FRACTURES</subject><subject>GEOLOGIC STRUCTURES</subject><subject>Geophysics</subject><subject>GEOSCIENCES</subject><subject>Intervals</subject><subject>LASERS</subject><subject>Mathematical analysis</subject><subject>MONITORING</subject><subject>NORTH AMERICA</subject><subject>PLATE TECTONICS</subject><subject>REMOTE SENSING</subject><subject>SATELLITES</subject><subject>Stability</subject><subject>Stations</subject><subject>STRATA MOVEMENT</subject><subject>TECTONICS</subject><subject>USA</subject><subject>Vectors (mathematics)</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1989</creationdate><recordtype>article</recordtype><sourceid>CYI</sourceid><recordid>eNqFkT1vFDEQhlcIJI5ATUNhUSCaTez117qMkrAEFgKXoCAaa9axOZM972H7BPfvcW4RBQVUHmue59WMpqqeEnxIcKOOuh4T4TEWG4w5VfeqBVGM1S3G8n61wFiVupHiYfUopW8YY4opWVTjErJFk0NmBeHrvsoriz5ufTC7-t0UtmsbMvpg4RYNkOzog0UuTmsEKEcIaZwMZD8FBAHGXfLpLqI_7s4uLlFfhIiW--BTyPC4euBgTPbJ7_eg-vTq7Orkdd1fdOcnx30NjEtVKyawlcrcuIHetMSW9YhjzrVusAOhRAhGJCg3OEkUKMm5kEYBiPLjQBU9qJ7PuVPKXifjszUrM4VgTdacK9VwWqAXM7SJ0_etTVmvfTJ2HCHYaZt0wxlTshEFfPlPkHCKVUsFIQU9mlETp5SidXoT_RriThOs766k_7pSMdhs_PCj3f0P192yZ3SvPZu1AAl0yLGMoVpVINYSXNr13PYp259_UiHeaiGp5Pr6fac_X_Kr6zdfmH5LfwGxjKrg</recordid><startdate>198906</startdate><enddate>198906</enddate><creator>Stolz, A.</creator><creator>Vincent, M. A.</creator><creator>Bender, P. L.</creator><creator>Eanes, R. J.</creator><creator>Watkins, M. M.</creator><creator>Tapley, B. D.</creator><general>Blackwell Publishing Ltd</general><scope>BSCLL</scope><scope>CYE</scope><scope>CYI</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7SP</scope><scope>7U5</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope><scope>OTOTI</scope></search><sort><creationdate>198906</creationdate><title>Rate of change of the Quincy-Monument Peak baseline from a translocation analysis of LAGEOS Laser Range Data</title><author>Stolz, A. ; Vincent, M. A. ; Bender, P. L. ; Eanes, R. J. ; Watkins, M. M. ; Tapley, B. 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D.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Rate of change of the Quincy-Monument Peak baseline from a translocation analysis of LAGEOS Laser Range Data</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>1989-06</date><risdate>1989</risdate><volume>16</volume><issue>6</issue><spage>539</spage><epage>542</epage><pages>539-542</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><abstract>Translocation studies of Lageos laser range data from Quincy and Monument Peak in California observed during 1984-1987 suggest that plate tectonic motion across the San Andreas fault system in the direction of the baseline between the two stations is uniform at a rate of -30(+ or - 3) mm/yr. Changes in the components of the baseline vector were inferred from repeat determinations using the solutions from successive 0.5-year intervals. The changes in the vertical and transverse components of the Quincy-Monument Peak baseline are -0.4(+ or - 5) mm/yr and +14(+ or -5) mm/yr, respectively. The vertical component determinations attest to the height stability of the laser ranging method. Lageos measurements made from Quincy and Monument Peak before 1984 are inaccurate enough to limit their usefulness for plate tectonic studies.</abstract><cop>Legacy CDMS</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/GL016i006p00539</doi><tpages>4</tpages></addata></record> |
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| ispartof | Geophysical research letters, 1989-06, Vol.16 (6), p.539-542 |
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| source | Wiley Online Library Journals Frontfile Complete; NASA Technical Reports Server |
| subjects | 580000 - Geosciences ACCURACY CALIFORNIA DEVELOPED COUNTRIES FEDERAL REGION IX GEOLOGIC FAULTS GEOLOGIC FRACTURES GEOLOGIC STRUCTURES Geophysics GEOSCIENCES Intervals LASERS Mathematical analysis MONITORING NORTH AMERICA PLATE TECTONICS REMOTE SENSING SATELLITES Stability Stations STRATA MOVEMENT TECTONICS USA Vectors (mathematics) |
| title | Rate of change of the Quincy-Monument Peak baseline from a translocation analysis of LAGEOS Laser Range Data |
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