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<!DOCTYPE ArticleSet PUBLIC "-//NLM//DTD PubMed 2.7//EN" "https://dtd.nlm.nih.gov/ncbi/pubmed/in/PubMed.dtd">
<ArticleSet>
<Article>
<Journal>
				<PublisherName>Damghan University Press</PublisherName>
				<JournalTitle>Iranian Journal of Astronomy and Astrophysics</JournalTitle>
				<Issn>2322-4924</Issn>
				<Volume>5</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2018</Year>
					<Month>04</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Slip distribution of the 2010 August 27 Mw 5.8 Kuh-Zar earthquake from ﬁnite-fault modeling</ArticleTitle>
<VernacularTitle>عنوان</VernacularTitle>
			<FirstPage>41</FirstPage>
			<LastPage>49</LastPage>
			<ELocationID EIdType="pii">141</ELocationID>
			
<ELocationID EIdType="doi">10.22128/ijaa.2018.141</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>Sonia </FirstName>
					<LastName>Bazargan</LastName>
<Affiliation>Institute of Geophysics, University of Tehran, Tehran, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Nazila </FirstName>
					<LastName>Asaadi</LastName>
<Affiliation>Physics Department, Zanjan University, Zanjan, Iran</Affiliation>
<Identifier Source="ORCID">0000-0001-5297-1237</Identifier>

</Author>
<Author>
					<FirstName>Zaher Hossein </FirstName>
					<LastName>Shomali</LastName>
<Affiliation>Institute of Geophysics, University of Tehran, Tehran, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Mehdi </FirstName>
					<LastName>Rezapour</LastName>
<Affiliation>Institute of Geophysics, University of Tehran, Tehran, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2019</Year>
					<Month>09</Month>
					<Day>15</Day>
				</PubDate>
			</History>
		<Abstract>The slip distribution of a moderate earthquake in Iran, the 27th of August, 2010 Mw 5 : 8 Kuh-Zar earthquake, was estimated from regional broadband seismic data using constrained non-negative least squares linear slip inversion method. A great many inversions were carried to determine the optimal parameters used in the process such as rupture velocity and rise time. A rupture velocity of 2.55 km/s and rise time of 1.8 s were utilized for the event. Results show a rupture with peak slip of 15.0 cm and total seismic moment release of 2 × 1025 dyne-cm. The eﬀect of the stations with diﬀerent epicentral distances was also analyzed using a sensitivity test. Due to the non-uniqueness of the inversion problem, a set of solutions is presented for the Kuh-Zar earthquake. To the best of our knowledge, this is the ﬁrst time to consider constrained non-negative least square linear ﬁnite-fault inversion procedure to the Kuh-Zar earthquake.&lt;br /&gt;  </Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">the 2010 Juh-Zar earthquake</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">seismic data</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">slip inversion</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://ijaa.du.ac.ir/article_141_a86ee530fe6b425e08efc8c8afb6670b.pdf</ArchiveCopySource>
</Article>
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