P-Wave Traveltime Analysis and Thomsen Parameters Inversion in Orthorhombic Media
An orthorhombic (ORT) model is the simplest azimuthally anisotropic model used to describe realistic fractured reservoirs (e.g., vertical cracks embedded in an anisotropic background media or orthogonal fracture systems in purely isotropic matrix). In this paper, we calculate the omnidirectional ref...
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Veröffentlicht in: | Chinese journal of geophysics 2005-09, Vol.48 (5), p.1247-1252 |
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creator | LU, Ming‐Hui TANG, Jian‐Hou YANG, Hui‐Zh HU, Bin |
description | An orthorhombic (ORT) model is the simplest azimuthally anisotropic model used to describe realistic fractured reservoirs (e.g., vertical cracks embedded in an anisotropic background media or orthogonal fracture systems in purely isotropic matrix). In this paper, we calculate the omnidirectional reflection traveltime of P‐wave in single orthorhombic media with horizontal interface by using the ray trace method. The reflection Pwave traveltime‐distance curves show strong azimuthal anisotropy. Using the Niche Genetic Algorithms (NGA), inversion of reflection traveltime of three common‐midpoint (CMP) lines provides us with a good estimation of azimuth, P‐ wave vertical velocity and Thomsen anisotropic parameters. |
doi_str_mv | 10.1002/cjg2.770 |
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Using the Niche Genetic Algorithms (NGA), inversion of reflection traveltime of three common‐midpoint (CMP) lines provides us with a good estimation of azimuth, P‐ wave vertical velocity and Thomsen anisotropic parameters.</description><identifier>ISSN: 0898-9591</identifier><identifier>EISSN: 2326-0440</identifier><identifier>DOI: 10.1002/cjg2.770</identifier><language>eng</language><publisher>Blackwell Publishing Ltd</publisher><subject>Anisotropic parameter ; Genetic Algorithm ; Orthorhombic ; Traveltime inversion</subject><ispartof>Chinese journal of geophysics, 2005-09, Vol.48 (5), p.1247-1252</ispartof><rights>2005 by the Chinese Geophysical Society</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a1710-5bfe978d02b0fcf890aa18e120a600e65ad95db288ac83b8feab0b8204bd9a193</citedby><cites>FETCH-LOGICAL-a1710-5bfe978d02b0fcf890aa18e120a600e65ad95db288ac83b8feab0b8204bd9a193</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>LU, Ming‐Hui</creatorcontrib><creatorcontrib>TANG, Jian‐Hou</creatorcontrib><creatorcontrib>YANG, Hui‐Zh</creatorcontrib><creatorcontrib>HU, Bin</creatorcontrib><title>P-Wave Traveltime Analysis and Thomsen Parameters Inversion in Orthorhombic Media</title><title>Chinese journal of geophysics</title><addtitle>Chinese J. Geophys</addtitle><description>An orthorhombic (ORT) model is the simplest azimuthally anisotropic model used to describe realistic fractured reservoirs (e.g., vertical cracks embedded in an anisotropic background media or orthogonal fracture systems in purely isotropic matrix). In this paper, we calculate the omnidirectional reflection traveltime of P‐wave in single orthorhombic media with horizontal interface by using the ray trace method. The reflection Pwave traveltime‐distance curves show strong azimuthal anisotropy. Using the Niche Genetic Algorithms (NGA), inversion of reflection traveltime of three common‐midpoint (CMP) lines provides us with a good estimation of azimuth, P‐ wave vertical velocity and Thomsen anisotropic parameters.</description><subject>Anisotropic parameter</subject><subject>Genetic Algorithm</subject><subject>Orthorhombic</subject><subject>Traveltime inversion</subject><issn>0898-9591</issn><issn>2326-0440</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2005</creationdate><recordtype>article</recordtype><recordid>eNp10E9PwjAYx_HGaCKiiS-hRy_Dp92_9kiIIAYEkwnH5unWSXEbpl1Q3r0jGBMPXp7f5ZPn8CXklsGAAfD7fPvGB2kKZ6THQ54EEEVwTnogpAhkLNklufJ-20kJEPXIyzJY497QzHW3am1t6LDB6uCtp9gUNNvsam8aukSHtWmN83Ta7Luxu4bahi5cu9m5Dmmb07kpLF6TixIrb25-tk9exw_Z6DGYLSbT0XAWIEsZBLEujUxFAVxDmZdCAiIThnHABMAkMRYyLjQXAnMRalEa1KAFh0gXEpkM--Tu9Dd3O--dKdWHszW6g2KgjinUMYXqUnQ0ONFPW5nDv06Nnib8j7e-NV-_Ht27StIwjdX6eaJWy2yejpNYrcJvhAFvlA</recordid><startdate>200509</startdate><enddate>200509</enddate><creator>LU, Ming‐Hui</creator><creator>TANG, Jian‐Hou</creator><creator>YANG, Hui‐Zh</creator><creator>HU, Bin</creator><general>Blackwell Publishing Ltd</general><scope>BSCLL</scope><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>200509</creationdate><title>P-Wave Traveltime Analysis and Thomsen Parameters Inversion in Orthorhombic Media</title><author>LU, Ming‐Hui ; TANG, Jian‐Hou ; YANG, Hui‐Zh ; HU, Bin</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a1710-5bfe978d02b0fcf890aa18e120a600e65ad95db288ac83b8feab0b8204bd9a193</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2005</creationdate><topic>Anisotropic parameter</topic><topic>Genetic Algorithm</topic><topic>Orthorhombic</topic><topic>Traveltime inversion</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>LU, Ming‐Hui</creatorcontrib><creatorcontrib>TANG, Jian‐Hou</creatorcontrib><creatorcontrib>YANG, Hui‐Zh</creatorcontrib><creatorcontrib>HU, Bin</creatorcontrib><collection>Istex</collection><collection>CrossRef</collection><jtitle>Chinese journal of geophysics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>LU, Ming‐Hui</au><au>TANG, Jian‐Hou</au><au>YANG, Hui‐Zh</au><au>HU, Bin</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>P-Wave Traveltime Analysis and Thomsen Parameters Inversion in Orthorhombic Media</atitle><jtitle>Chinese journal of geophysics</jtitle><addtitle>Chinese J. Geophys</addtitle><date>2005-09</date><risdate>2005</risdate><volume>48</volume><issue>5</issue><spage>1247</spage><epage>1252</epage><pages>1247-1252</pages><issn>0898-9591</issn><eissn>2326-0440</eissn><abstract>An orthorhombic (ORT) model is the simplest azimuthally anisotropic model used to describe realistic fractured reservoirs (e.g., vertical cracks embedded in an anisotropic background media or orthogonal fracture systems in purely isotropic matrix). In this paper, we calculate the omnidirectional reflection traveltime of P‐wave in single orthorhombic media with horizontal interface by using the ray trace method. The reflection Pwave traveltime‐distance curves show strong azimuthal anisotropy. Using the Niche Genetic Algorithms (NGA), inversion of reflection traveltime of three common‐midpoint (CMP) lines provides us with a good estimation of azimuth, P‐ wave vertical velocity and Thomsen anisotropic parameters.</abstract><pub>Blackwell Publishing Ltd</pub><doi>10.1002/cjg2.770</doi><tpages>6</tpages></addata></record> |
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subjects | Anisotropic parameter Genetic Algorithm Orthorhombic Traveltime inversion |
title | P-Wave Traveltime Analysis and Thomsen Parameters Inversion in Orthorhombic Media |
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