<?xml version="1.0" encoding="ISO-8859-1"?>
<metadatalist>
	<metadata ReferenceType="Conference Proceedings">
		<site>mtc-m12.sid.inpe.br 800</site>
		<holdercode>{isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S}</holdercode>
		<identifier>6qtX3pFwXQZ3r59YD6/GP7Vk</identifier>
		<repository>sid.inpe.br/iris@1912/2005/07.20.03.12</repository>
		<lastupdate>2015:12.14.14.47.21 sid.inpe.br/banon/2001/04.06.10.52 marciana</lastupdate>
		<metadatarepository>sid.inpe.br/iris@1912/2005/07.20.03.12.30</metadatarepository>
		<metadatalastupdate>2024:11.06.18.26.04 sid.inpe.br/banon/2001/04.06.10.52 marciana {D 1994}</metadatalastupdate>
		<secondarykey>INPE-7629-PRE/3479</secondarykey>
		<label>6819</label>
		<citationkey>AnjosVene:1994:EWLiPa</citationkey>
		<title>The EW-NS lineament pattern recognizes in structural analysus using remote sensing products and is control over terrains of the brazilian craton</title>
		<year>1994</year>
		<secondarytype>PRE CI</secondarytype>
		<numberoffiles>1</numberoffiles>
		<size>4925 KiB</size>
		<author>Anjos, C. E.,</author>
		<author>Veneziani, P.,</author>
		<group>DSM-INPE-MCT-BR</group>
		<conferencename>Thematic Conference on Geologic Remote Sensing, 10.</conferencename>
		<conferencelocation>San Antonio, Texas, USA</conferencelocation>
		<date>09-12 May 1994</date>
		<pages>372-</pages>
		<transferableflag>1</transferableflag>
		<contenttype>External Contribution</contenttype>
		<keywords>GEOLOGIA.</keywords>
		<abstract>A pervasive NS-EW patern of structural lineaments on Brazilian terrains has been identified on remote sensing products.Such pattern can befound by cutting ando controlling rocks as well as and structures from the Archean to the Paleozoic ages. These rocks have been under several deformation cycles. Those NS and EW structural lineaments exert paleogeogreaphic, sedimentological and tectogenetifal control over several litho-structural units. They appear in a subtle way in satellite images, as a direction of maximum density of other fractural patterns. The NS-EW pattern reveals its policyclic character and its influence on the strucutural evolution of the Brazilian craton.</abstract>
		<area>SRE</area>
		<targetfile>INPE 7629.pdf</targetfile>
		<usergroup>administrator</usergroup>
		<usergroup>marciana</usergroup>
		<visibility>shown</visibility>
		<readpermission>allow from all</readpermission>
		<documentstage>not transferred</documentstage>
		<nexthigherunit>8JMKD3MGPCW/46JL46L</nexthigherunit>
		<citingitemlist>sid.inpe.br/bibdigital/2022/03.26.21.39 8</citingitemlist>
		<hostcollection>sid.inpe.br/banon/2001/04.06.10.52</hostcollection>
		<username>marciana</username>
		<lasthostcollection>sid.inpe.br/banon/2001/04.06.10.52</lasthostcollection>
		<url>http://mtc-m12.sid.inpe.br/rep-/sid.inpe.br/iris@1912/2005/07.20.03.12</url>
	</metadata>
</metadatalist>