{"title":"西伯罗奔尼撒近海:希腊北部伊奥尼亚的结构元素和差异","authors":"V. Kosmidou, S. Bellas, Y. Bassias","doi":"10.3997/2214-4609.201803039","DOIUrl":null,"url":null,"abstract":"This paper suggests that the carbonate units south of the Kefalonia Transform Zone (KTZ) (Scordilis et al., 1985) bear similarities to the northern Paxi formations. From North to South and crossing the KTZ, we encounter sharply, from the Apulian Platform north of the KTZ, the Mediterranean Ridge, the backstop, the Hellenic Trench and the Hellenides Thrust and Fold Belt (TFB), south of the KTZ. Interpretation of data based on the 2012-2013 MC 2D seismic acquisition of PGS.","PeriodicalId":213700,"journal":{"name":"Eastern Mediterranean Workshop 2018","volume":"127 2 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2018-12-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Offshore Western Peloponnese: Structural Elements And Differences From Northern Ionian, Greece\",\"authors\":\"V. Kosmidou, S. Bellas, Y. Bassias\",\"doi\":\"10.3997/2214-4609.201803039\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"This paper suggests that the carbonate units south of the Kefalonia Transform Zone (KTZ) (Scordilis et al., 1985) bear similarities to the northern Paxi formations. From North to South and crossing the KTZ, we encounter sharply, from the Apulian Platform north of the KTZ, the Mediterranean Ridge, the backstop, the Hellenic Trench and the Hellenides Thrust and Fold Belt (TFB), south of the KTZ. Interpretation of data based on the 2012-2013 MC 2D seismic acquisition of PGS.\",\"PeriodicalId\":213700,\"journal\":{\"name\":\"Eastern Mediterranean Workshop 2018\",\"volume\":\"127 2 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2018-12-06\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Eastern Mediterranean Workshop 2018\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.3997/2214-4609.201803039\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Eastern Mediterranean Workshop 2018","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.3997/2214-4609.201803039","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
摘要
本文认为，Kefalonia转换带(KTZ)以南的碳酸盐岩单元(Scordilis et al.， 1985)与北部的Paxi组具有相似性。从北到南，穿过KTZ，我们从KTZ以北的阿普利亚台地，地中海山脊，后方，希腊海沟和KTZ以南的Hellenides逆冲和褶皱带(TFB)尖锐地遇到。基于PGS 2012-2013年MC 2D地震采集数据的解释
Offshore Western Peloponnese: Structural Elements And Differences From Northern Ionian, Greece
This paper suggests that the carbonate units south of the Kefalonia Transform Zone (KTZ) (Scordilis et al., 1985) bear similarities to the northern Paxi formations. From North to South and crossing the KTZ, we encounter sharply, from the Apulian Platform north of the KTZ, the Mediterranean Ridge, the backstop, the Hellenic Trench and the Hellenides Thrust and Fold Belt (TFB), south of the KTZ. Interpretation of data based on the 2012-2013 MC 2D seismic acquisition of PGS.
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