Morphometric analysis of small-scale lobate scarps on the Moon using data from the Lunar Reconnaissance Orbiter
Prior to Lunar Reconnaissance Orbiter (LRO), the morphology and dimensions of only a limited number of lobate scarps, all located near the equator (within 21°), had been characterized. Topography derived from LRO Camera stereo images and Lunar Orbiter Laser Altimeter (LOLA) ranging is used to measur...
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creator | Banks, M. E. Watters, T. R. Robinson, M. S. Tornabene, L. L. Tran, T. Ojha, L. Williams, N. R. |
description | Prior to Lunar Reconnaissance Orbiter (LRO), the morphology and dimensions of only a limited number of lobate scarps, all located near the equator (within 21°), had been characterized. Topography derived from LRO Camera stereo images and Lunar Orbiter Laser Altimeter (LOLA) ranging is used to measure the relief and analyze the morphology of previously known and newly detected low and high latitude lobate scarps. The asymmetric profiles and maximum slopes on scarp faces (∼5° to 29°) of lunar lobate scarps are similar to those of lobate scarps observed on Mars and Mercury. Scarp lengths range from ∼0.6 to 21.6 km (mean = ∼6.0 km, median = ∼4.4 km, n = 79), and measured relief ranges from ∼5 to 150 m (mean = ∼35 m, median = ∼20 m, n = 26). Assuming a range of 20° to 40° for the fault plane dip, estimated lower limits for the horizontal shortening (S) expressed by the lobate scarp thrust faults range from ∼10 to 410 m. The range in S estimated for the lunar scarps is roughly an order of magnitude lower than estimates of S for lobate scarp thrust faults on Mars and Mercury. The relatively small range of S estimated for the growing number of well‐characterized lunar scarps is consistent with a small amount of global contraction.
Key Points
Analysis of lunar lobate scarp morphology
Comparison of lunar lobate scarps to lobate scarps on Mars, Mercury, and Eros
Analysis of the horizontal shortening expressed by lunar lobate scarps |
doi_str_mv | 10.1029/2011JE003907 |
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Key Points
Analysis of lunar lobate scarp morphology
Comparison of lunar lobate scarps to lobate scarps on Mars, Mercury, and Eros
Analysis of the horizontal shortening expressed by lunar lobate scarps</description><identifier>ISSN: 0148-0227</identifier><identifier>ISSN: 2169-9097</identifier><identifier>EISSN: 2156-2202</identifier><identifier>EISSN: 2169-9100</identifier><identifier>DOI: 10.1029/2011JE003907</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Equator ; lobate scarps ; Mercury ; Moon ; morphology ; Planetology ; Planets ; Remote sensing ; tectonics</subject><ispartof>Journal of Geophysical Research: Planets, 2012, Vol.117 (E12), p.n/a</ispartof><rights>2012 by the American Geophysical Union</rights><rights>Copyright 2012 by the American Geophysical Union</rights><rights>Copyright American Geophysical Union 2012</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a5325-273023af6f8515abd7734a9b35d4637ff8a484b6e3ee482b77e2055345785a6e3</citedby><cites>FETCH-LOGICAL-a5325-273023af6f8515abd7734a9b35d4637ff8a484b6e3ee482b77e2055345785a6e3</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%2F2011JE003907$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2011JE003907$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,1427,4010,11493,27900,27901,27902,45550,45551,46384,46443,46808,46867</link.rule.ids></links><search><creatorcontrib>Banks, M. E.</creatorcontrib><creatorcontrib>Watters, T. R.</creatorcontrib><creatorcontrib>Robinson, M. S.</creatorcontrib><creatorcontrib>Tornabene, L. L.</creatorcontrib><creatorcontrib>Tran, T.</creatorcontrib><creatorcontrib>Ojha, L.</creatorcontrib><creatorcontrib>Williams, N. R.</creatorcontrib><title>Morphometric analysis of small-scale lobate scarps on the Moon using data from the Lunar Reconnaissance Orbiter</title><title>Journal of Geophysical Research: Planets</title><addtitle>J. Geophys. Res</addtitle><description>Prior to Lunar Reconnaissance Orbiter (LRO), the morphology and dimensions of only a limited number of lobate scarps, all located near the equator (within 21°), had been characterized. Topography derived from LRO Camera stereo images and Lunar Orbiter Laser Altimeter (LOLA) ranging is used to measure the relief and analyze the morphology of previously known and newly detected low and high latitude lobate scarps. The asymmetric profiles and maximum slopes on scarp faces (∼5° to 29°) of lunar lobate scarps are similar to those of lobate scarps observed on Mars and Mercury. Scarp lengths range from ∼0.6 to 21.6 km (mean = ∼6.0 km, median = ∼4.4 km, n = 79), and measured relief ranges from ∼5 to 150 m (mean = ∼35 m, median = ∼20 m, n = 26). Assuming a range of 20° to 40° for the fault plane dip, estimated lower limits for the horizontal shortening (S) expressed by the lobate scarp thrust faults range from ∼10 to 410 m. The range in S estimated for the lunar scarps is roughly an order of magnitude lower than estimates of S for lobate scarp thrust faults on Mars and Mercury. The relatively small range of S estimated for the growing number of well‐characterized lunar scarps is consistent with a small amount of global contraction.
Key Points
Analysis of lunar lobate scarp morphology
Comparison of lunar lobate scarps to lobate scarps on Mars, Mercury, and Eros
Analysis of the horizontal shortening expressed by lunar lobate scarps</description><subject>Equator</subject><subject>lobate scarps</subject><subject>Mercury</subject><subject>Moon</subject><subject>morphology</subject><subject>Planetology</subject><subject>Planets</subject><subject>Remote sensing</subject><subject>tectonics</subject><issn>0148-0227</issn><issn>2169-9097</issn><issn>2156-2202</issn><issn>2169-9100</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kU1vFDEMhiNEJValN35AJC4cGMjnJHNEq-2W1ZZKbRESl8gz66EpmcmSzAj235OyCKEe6ovt-LHfyCbkFWfvOBPNe8E436wYkw0zz8hCcF1XQjDxnCwYV7ZiQpgX5Czne1ZM6VoxviDxMqb9XRxwSr6jMEI4ZJ9p7GkeIIQqdxCQhtjChLQkaV-KI53ukF7GEszZj9_oDiagfYrDn8J2HiHRa-ziOILPGcYO6VVq_YTpJTnpIWQ8--tPyefz1e3yotperT8uP2wr0FLoShjJhIS-7q3mGtqdMVJB00q9U7U0fW9BWdXWKBGVFa0xKJjWUmljNZTnU_LmOHef4o8Z8-QGnzsMAUaMc3ZlZaqumWVNQV8_Qu_jnMomCsWFFJaz2jxNcW2tUbUu1Nsj1aWYc8Le7ZMfIB2K4INm4_4_U8HFEf_pAx6eZN1mfb0SjX3QqI5NPk_4618TpO-u_NNo9-XT2i03W3Fjv547JX8DXFmgJQ</recordid><startdate>2012</startdate><enddate>2012</enddate><creator>Banks, M. 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L. ; Tran, T. ; Ojha, L. ; Williams, N. R.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a5325-273023af6f8515abd7734a9b35d4637ff8a484b6e3ee482b77e2055345785a6e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>Equator</topic><topic>lobate scarps</topic><topic>Mercury</topic><topic>Moon</topic><topic>morphology</topic><topic>Planetology</topic><topic>Planets</topic><topic>Remote sensing</topic><topic>tectonics</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Banks, M. E.</creatorcontrib><creatorcontrib>Watters, T. R.</creatorcontrib><creatorcontrib>Robinson, M. S.</creatorcontrib><creatorcontrib>Tornabene, L. L.</creatorcontrib><creatorcontrib>Tran, T.</creatorcontrib><creatorcontrib>Ojha, L.</creatorcontrib><creatorcontrib>Williams, N. 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E.</au><au>Watters, T. R.</au><au>Robinson, M. S.</au><au>Tornabene, L. L.</au><au>Tran, T.</au><au>Ojha, L.</au><au>Williams, N. R.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Morphometric analysis of small-scale lobate scarps on the Moon using data from the Lunar Reconnaissance Orbiter</atitle><jtitle>Journal of Geophysical Research: Planets</jtitle><addtitle>J. Geophys. Res</addtitle><date>2012</date><risdate>2012</risdate><volume>117</volume><issue>E12</issue><epage>n/a</epage><issn>0148-0227</issn><issn>2169-9097</issn><eissn>2156-2202</eissn><eissn>2169-9100</eissn><abstract>Prior to Lunar Reconnaissance Orbiter (LRO), the morphology and dimensions of only a limited number of lobate scarps, all located near the equator (within 21°), had been characterized. Topography derived from LRO Camera stereo images and Lunar Orbiter Laser Altimeter (LOLA) ranging is used to measure the relief and analyze the morphology of previously known and newly detected low and high latitude lobate scarps. The asymmetric profiles and maximum slopes on scarp faces (∼5° to 29°) of lunar lobate scarps are similar to those of lobate scarps observed on Mars and Mercury. Scarp lengths range from ∼0.6 to 21.6 km (mean = ∼6.0 km, median = ∼4.4 km, n = 79), and measured relief ranges from ∼5 to 150 m (mean = ∼35 m, median = ∼20 m, n = 26). Assuming a range of 20° to 40° for the fault plane dip, estimated lower limits for the horizontal shortening (S) expressed by the lobate scarp thrust faults range from ∼10 to 410 m. The range in S estimated for the lunar scarps is roughly an order of magnitude lower than estimates of S for lobate scarp thrust faults on Mars and Mercury. The relatively small range of S estimated for the growing number of well‐characterized lunar scarps is consistent with a small amount of global contraction.
Key Points
Analysis of lunar lobate scarp morphology
Comparison of lunar lobate scarps to lobate scarps on Mars, Mercury, and Eros
Analysis of the horizontal shortening expressed by lunar lobate scarps</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2011JE003907</doi><tpages>11</tpages><oa>free_for_read</oa></addata></record> |
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source | Wiley-Blackwell AGU Digital Library; Wiley Online Library Journals Frontfile Complete; Wiley Online Library Free Content; Alma/SFX Local Collection |
subjects | Equator lobate scarps Mercury Moon morphology Planetology Planets Remote sensing tectonics |
title | Morphometric analysis of small-scale lobate scarps on the Moon using data from the Lunar Reconnaissance Orbiter |
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