LIVELLI CALCAREI CLASTICI DEL MIOCENE SUPERIORE E PLIOCENE NEL SOTTOSUOLO MOLISANO-PUGLIESE

IF 1.6 3区 地球科学 Q2 GEOLOGY Rivista Italiana Di Paleontologia E Stratigrafia Pub Date : 2020-05-08 DOI:10.54103/2039-4942/13431
R. Casnedi, A. Balduzzi
{"title":"LIVELLI CALCAREI CLASTICI DEL MIOCENE SUPERIORE E PLIOCENE NEL SOTTOSUOLO MOLISANO-PUGLIESE","authors":"R. Casnedi, A. Balduzzi","doi":"10.54103/2039-4942/13431","DOIUrl":null,"url":null,"abstract":"The Molise and Apulia subsurface exploration has found clastic calcareous layers at the top of the Mesozoic—Miocene carbonate sequence and within the Middle Pliocene turbidites. The first are the result of Karst—fissures and crushing on the structural highs and mass flows at the base of fault slopes. Within the turbidites a biocalcarenitic horizon IS an electric good marker which proves an event of a shelf build up. It corresponds to the Middle Pliocene gap widely developed in the Apennines.","PeriodicalId":54451,"journal":{"name":"Rivista Italiana Di Paleontologia E Stratigrafia","volume":null,"pages":null},"PeriodicalIF":1.6000,"publicationDate":"2020-05-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Rivista Italiana Di Paleontologia E Stratigrafia","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.54103/2039-4942/13431","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOLOGY","Score":null,"Total":0}
引用次数: 0

Abstract

The Molise and Apulia subsurface exploration has found clastic calcareous layers at the top of the Mesozoic—Miocene carbonate sequence and within the Middle Pliocene turbidites. The first are the result of Karst—fissures and crushing on the structural highs and mass flows at the base of fault slopes. Within the turbidites a biocalcarenitic horizon IS an electric good marker which proves an event of a shelf build up. It corresponds to the Middle Pliocene gap widely developed in the Apennines.
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
莫利塞-阿普利亚底土中的上新世和上新世碎屑灰岩层
莫利塞和阿普利亚地下勘探在中生代-中新世碳酸盐序列顶部和中新世浊积岩内发现了碎屑钙质层。前者是喀斯特裂隙和构造高地挤压的结果,后者是断层斜坡底部大量流动的结果。在浊积岩中,一个生物钙钛矿地层是一个很好的电标记,证明了陆架的形成。它与亚平宁山脉广泛发育的中新世缺口相对应。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 去求助
来源期刊
CiteScore
3.60
自引率
4.30%
发文量
28
审稿时长
>12 weeks
期刊介绍: The Rivista Italiana di Paleontologia e Stratigrafia was founded in 1895. It publishes original papers dealing with all fields of paleontology and of stratigraphy, from Italy and the Mediterranean to the Tethys, as well across the globe from China to North America.
期刊最新文献
NEW ACROPOMATIFORM FOSSILS FROM THE UPPER KUEICHULIN FORMATION (LOWER PLIOCENE), NORTHERN TAIWAN REVISITING THE CRETACEOUS LUNGFISH ATLANTOCERATODUS IHERINGI (AMEGHINO 1898) FROM THE MATA AMARILLA FORMATION (ARGENTINA) WITH COMMENTS ON TOOTH PLATES HISTOLOGY FIRST REPORT ON THE UPPERMOST PERMIAN OSTRACODS FROM THE MASORE SECTION (EXTERNAL DINARIDES), SLOVENIA EOCENE STALKED CRINOIDS IN THE GENUS ISSELICRINUS (ECHINODERMATA, CRINOIDEA, ISOCRINIDA) FROM NORTHEASTERN ITALY NEW REPORT OF DECAPOD AND ISOPOD CRUSTACEANS FROM THE LOWERMIDDLE PLEISTOCENE OF MONTALBANO JONICO, MATERA (BASILICATA, SOUTHERN ITALY)
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1