Structure and its impact in Uthangarai and Thirthamalai region, Tamil Nadu, India using remote sensing technique
The Uthangarai-Thirthamalai region in Dharmapuri district is a typical Precambrian tract in Tamil Nadu. IRS-1C satellite imagery was used for interpreting folds, faults, fractures and lineaments, in this region. As interpreted from the satellite imagery, there are five major structural domains, whic...
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Veröffentlicht in: | Journal of the Indian Society of Remote Sensing 2001-12, Vol.29 (4), p.187-195 |
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description | The Uthangarai-Thirthamalai region in Dharmapuri district is a typical Precambrian tract in Tamil Nadu. IRS-1C satellite imagery was used for interpreting folds, faults, fractures and lineaments, in this region. As interpreted from the satellite imagery, there are five major structural domains, which control the Ponnaiyar, Pambar, Vaniyar and Kovilar river courses and other drainage pattern in this region. Presence of fault rock, epidotization and sympathetic fractures along such folds and faults reveals the intensity of tectonism in this sector. The interpreted lineaments have been classified into five major groups on the basis of their geometry and orientation. From the rose diagram, it is inferred that the NNW-SSE trending lineaments are fall in major frequency domain. The springs observed near Hanumanthirtham and Thirthamalai region could be structurally originated. The geomorphology interpreted from the satellite data has shown significant morphological expression of folds, faults and lineaments. The geophysical data have been analysed and correlated with intensity of weathering by fractures and lineaments. |
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IRS-1C satellite imagery was used for interpreting folds, faults, fractures and lineaments, in this region. As interpreted from the satellite imagery, there are five major structural domains, which control the Ponnaiyar, Pambar, Vaniyar and Kovilar river courses and other drainage pattern in this region. Presence of fault rock, epidotization and sympathetic fractures along such folds and faults reveals the intensity of tectonism in this sector. The interpreted lineaments have been classified into five major groups on the basis of their geometry and orientation. From the rose diagram, it is inferred that the NNW-SSE trending lineaments are fall in major frequency domain. The springs observed near Hanumanthirtham and Thirthamalai region could be structurally originated. The geomorphology interpreted from the satellite data has shown significant morphological expression of folds, faults and lineaments. The geophysical data have been analysed and correlated with intensity of weathering by fractures and lineaments.</description><identifier>ISSN: 0255-660X</identifier><identifier>EISSN: 0974-3006</identifier><identifier>DOI: 10.1007/BF02995723</identifier><language>eng</language><publisher>Dordrecht: Springer Nature B.V</publisher><subject>Drainage patterns ; Faults ; Fractures ; Geomorphology ; Precambrian ; Remote sensing ; Satellite imagery ; Satellites ; Springs (elastic)</subject><ispartof>Journal of the Indian Society of Remote Sensing, 2001-12, Vol.29 (4), p.187-195</ispartof><rights>Springer-Verlag 2001.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a197t-96943e7d5efd7c1e8fc6504d5ea8c0eea1feb6accc89fa5fb34f05efcaebd6503</citedby><cites>FETCH-LOGICAL-a197t-96943e7d5efd7c1e8fc6504d5ea8c0eea1feb6accc89fa5fb34f05efcaebd6503</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Anbazhagan, S</creatorcontrib><creatorcontrib>Saranathan, E</creatorcontrib><title>Structure and its impact in Uthangarai and Thirthamalai region, Tamil Nadu, India using remote sensing technique</title><title>Journal of the Indian Society of Remote Sensing</title><description>The Uthangarai-Thirthamalai region in Dharmapuri district is a typical Precambrian tract in Tamil Nadu. IRS-1C satellite imagery was used for interpreting folds, faults, fractures and lineaments, in this region. As interpreted from the satellite imagery, there are five major structural domains, which control the Ponnaiyar, Pambar, Vaniyar and Kovilar river courses and other drainage pattern in this region. Presence of fault rock, epidotization and sympathetic fractures along such folds and faults reveals the intensity of tectonism in this sector. The interpreted lineaments have been classified into five major groups on the basis of their geometry and orientation. From the rose diagram, it is inferred that the NNW-SSE trending lineaments are fall in major frequency domain. The springs observed near Hanumanthirtham and Thirthamalai region could be structurally originated. The geomorphology interpreted from the satellite data has shown significant morphological expression of folds, faults and lineaments. The geophysical data have been analysed and correlated with intensity of weathering by fractures and lineaments.</description><subject>Drainage patterns</subject><subject>Faults</subject><subject>Fractures</subject><subject>Geomorphology</subject><subject>Precambrian</subject><subject>Remote sensing</subject><subject>Satellite imagery</subject><subject>Satellites</subject><subject>Springs (elastic)</subject><issn>0255-660X</issn><issn>0974-3006</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2001</creationdate><recordtype>article</recordtype><recordid>eNpFUF1LwzAUDaLgnL74CwK-yapJ2zTto45NB0Mf3MC3cpfebBlrWpP0wX9v3AThwr3ng3vgEHLL2QNnTD4-z1laVUKm2RkZsUrmScZYcR7vVIikKNjnJbnyfh_JXPB0RPqP4AYVBocUbENN8NS0PahAjaXrsAO7BQfmKK52xkWmhUMkHG5NZyd0Ba050Ddohgld2MYAHbyx26i3XUDq0R5hQLWz5mvAa3Kh4eDx5m-PyXo-W01fk-X7y2L6tEyAVzIkVVHlGcpGoG6k4lhqVQiWRwylYojANW4KUEqVlQahN1muWTQrwE0TndmY3J3-9q6LsT7U-25wNkbWqSxlKsoszpjcn1zKdd471HXvTAvuu-as_m20_m80-wHJqGrj</recordid><startdate>200112</startdate><enddate>200112</enddate><creator>Anbazhagan, S</creator><creator>Saranathan, E</creator><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>200112</creationdate><title>Structure and its impact in Uthangarai and Thirthamalai region, Tamil Nadu, India using remote sensing technique</title><author>Anbazhagan, S ; Saranathan, E</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a197t-96943e7d5efd7c1e8fc6504d5ea8c0eea1feb6accc89fa5fb34f05efcaebd6503</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2001</creationdate><topic>Drainage patterns</topic><topic>Faults</topic><topic>Fractures</topic><topic>Geomorphology</topic><topic>Precambrian</topic><topic>Remote sensing</topic><topic>Satellite imagery</topic><topic>Satellites</topic><topic>Springs (elastic)</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Anbazhagan, S</creatorcontrib><creatorcontrib>Saranathan, E</creatorcontrib><collection>CrossRef</collection><jtitle>Journal of the Indian Society of Remote Sensing</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Anbazhagan, S</au><au>Saranathan, E</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Structure and its impact in Uthangarai and Thirthamalai region, Tamil Nadu, India using remote sensing technique</atitle><jtitle>Journal of the Indian Society of Remote Sensing</jtitle><date>2001-12</date><risdate>2001</risdate><volume>29</volume><issue>4</issue><spage>187</spage><epage>195</epage><pages>187-195</pages><issn>0255-660X</issn><eissn>0974-3006</eissn><abstract>The Uthangarai-Thirthamalai region in Dharmapuri district is a typical Precambrian tract in Tamil Nadu. IRS-1C satellite imagery was used for interpreting folds, faults, fractures and lineaments, in this region. As interpreted from the satellite imagery, there are five major structural domains, which control the Ponnaiyar, Pambar, Vaniyar and Kovilar river courses and other drainage pattern in this region. Presence of fault rock, epidotization and sympathetic fractures along such folds and faults reveals the intensity of tectonism in this sector. The interpreted lineaments have been classified into five major groups on the basis of their geometry and orientation. From the rose diagram, it is inferred that the NNW-SSE trending lineaments are fall in major frequency domain. The springs observed near Hanumanthirtham and Thirthamalai region could be structurally originated. The geomorphology interpreted from the satellite data has shown significant morphological expression of folds, faults and lineaments. 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subjects | Drainage patterns Faults Fractures Geomorphology Precambrian Remote sensing Satellite imagery Satellites Springs (elastic) |
title | Structure and its impact in Uthangarai and Thirthamalai region, Tamil Nadu, India using remote sensing technique |
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