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<Article>
<Journal>
				<PublisherName>Shahid Beheshti University</PublisherName>
				<JournalTitle>Researches in Earth Sciences</JournalTitle>
				<Issn>2008-8299</Issn>
				<Volume>6</Volume>
				<Issue>4</Issue>
				<PubDate PubStatus="epublish">
					<Year>2015</Year>
					<Month>10</Month>
					<Day>23</Day>
				</PubDate>
			</Journal>
<ArticleTitle>The study of statistical models and fractal array fractures in the eastern Bajestan granite mass based on remote sensing techniques</ArticleTitle>
<VernacularTitle>The study of statistical models and fractal array fractures in the eastern Bajestan granite mass based on remote sensing techniques</VernacularTitle>
			<FirstPage>1</FirstPage>
			<LastPage>15</LastPage>
			<ELocationID EIdType="pii">95715</ELocationID>
			
			
			<Language>FA</Language>
<AuthorList>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2015</Year>
					<Month>05</Month>
					<Day>23</Day>
				</PubDate>
			</History>
		<Abstract>Analysis of intensity (I), Density (ρ), Mean lineament trace length (µ) and intersection (n), are the parameters used in the statistical calculations faults and fractures that are expressed per unit area. In this study, enhancement of lineaments has been done with the use of SPOT 5 image. Fractures were classified in two systematic trend northwest - southeast that are the dominant area trend and northeast – southwest. According to the area and the distribution of fractures, Area is divided to 42 square network with a side length of 1.7 kilometers. Then the fractal model of structural fractures area was calculated, the highest in southeast and west region was obtained. The above parameters for each network was calculated separately and manual and their contour maps were drawn. The highest I and ρ in southeast, west and the highest µ and n in the northeast and southeast region were obtained respectively.</Abstract>
			<OtherAbstract Language="FA">Analysis of intensity (I), Density (ρ), Mean lineament trace length (µ) and intersection (n), are the parameters used in the statistical calculations faults and fractures that are expressed per unit area. In this study, enhancement of lineaments has been done with the use of SPOT 5 image. Fractures were classified in two systematic trend northwest - southeast that are the dominant area trend and northeast – southwest. According to the area and the distribution of fractures, Area is divided to 42 square network with a side length of 1.7 kilometers. Then the fractal model of structural fractures area was calculated, the highest in southeast and west region was obtained. The above parameters for each network was calculated separately and manual and their contour maps were drawn. The highest I and ρ in southeast, west and the highest µ and n in the northeast and southeast region were obtained respectively.</OtherAbstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Bajestan granite- Remote sensing- Fractal- Spot 5</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://esrj.sbu.ac.ir/article_95715_3bdae368d1a3e255c81b7f262ba1bbf6.pdf</ArchiveCopySource>
</Article>
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