发布求助
文献互助 智能选刊 最新文献

Journal of iberian geology: an international publication of earth sciences最新文献

筛选
英文 中文
Structuration permienne du bassin Blanzy-Le Creusot et évolution pos-hercynienne. 布兰齐-勒克鲁索盆地二叠纪构造与后海西演化。
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1992.V16.2609
P. Debriette
{"title":"Structuration permienne du bassin Blanzy-Le Creusot et évolution pos-hercynienne.","authors":"P. Debriette","doi":"10.5209/REV_CGIB.1992.V16.2609","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1992.V16.2609","url":null,"abstract":"This study is based on tite lititostratigrapitie reconnaissance of tite whole outcrops of tite Blanzy-Le Creusot basin, completed by studying sections files, sismies lines, gravimetric maps and rnicrotectonic analysis of 21 outcrops. Tite","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"37 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"131562043","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Late Variscan events in the outer Ligurian Briançonnais. 外利古里亚布里阿<s:1>尼奥纳斯的晚期瓦利斯会事件。
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1992.V16.2615
R. Cabella, L. Cortesogno, G. Dallagiovanna, R. Vannucci, M. Vanossi
{"title":"Late Variscan events in the outer Ligurian Briançonnais.","authors":"R. Cabella, L. Cortesogno, G. Dallagiovanna, R. Vannucci, M. Vanossi","doi":"10.5209/REV_CGIB.1992.V16.2615","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1992.V16.2615","url":null,"abstract":"In ihe Ligurian Brian9onnais domain a late Variscan sequence of volcanie, mainly ignimbritic, and sedimentary continental deposits filled up graben and halfgraben struciures,bordered by two seis of syngeneticfaults (presently trendingnearlyE-Wand N-S), during tree man phases. The oldestone,ofWestphalian-Siephanian age, was accompanied by calc-alkaline rhyolite; ihe second one, of middle (7) Siephanian age, is marked by «shoshonitic» andesites; te last, early Permian one, gaye buge volumesof calc-alkaline rhyolitic to dacitic volcanics and was closed by a K-rhyolitic event. No volcanism is associaied with te uncamformably overlying late Permian continental coarse deposiis (Verrucano).","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"72 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"134584867","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 1
Estructura del borde N de la Cordillera Ibérica entre la Sierra de Arcos y el anticlinal de Montalbán 在Sierra de Arcos和montalban背斜之间的伊比利亚山脉N边缘的结构
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1997.V23.2494
A. Meléndez, A. C. Sáinz, Á. L. C. Gracia, A. R. Soria, Carlos L. Liesa
{"title":"Estructura del borde N de la Cordillera Ibérica entre la Sierra de Arcos y el anticlinal de Montalbán","authors":"A. Meléndez, A. C. Sáinz, Á. L. C. Gracia, A. R. Soria, Carlos L. Liesa","doi":"10.5209/REV_CGIB.1997.V23.2494","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1997.V23.2494","url":null,"abstract":"The Tertiary structure of the northern margin of the Iberian Chain between the Sierra de Arcos and the Montalban anticline is controlled by both the orientation of the Mesozoic extensional fauits and by the regional detachment levels in the Mesozoic cover and Palaeozoic basement. During the Mesozoic extension, two stages can be defined: 1) during the Valanginian-Hauterivian, the normal faults at the northern part, near the Sierra de Arcos high (with hangingwalls to the south) wcre associated with large roli-over anticlines in the marine Jurassic series, erosion of the latter being more important toward the south. 2) From Barremian times, the southern faults delimitting the Oliete Subbasin (hangingwalls to the north) were active, giving maximum sediment thickness near the Montalban anticline, which was a sedimentary high during ali the Early Crctaccous. A NE-SW fault set (with hangingwalls to thc SE) was responsible for changes of sediment thickness in the central part of the basin during the Early Cretaceous. The Tertiary NWSE (and some of the E-W and NE-SW) folds and thrusts, associated to alluvial fan syn-tectonic sedimentation, were the result of positive inversion of Mesozoic normal faults.","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"15 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"134523689","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 12
Evolución y características sedimentológicas de las facies fluviales basales del Buntsandstein de Olesa de Montserrat (Provincia de Barcelona). 巴塞罗那省Olesa de Montserrat Buntsandstein河基相的演化和沉积特征。
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1977.V4.2891
P. Monzón, M. M. Carpio
{"title":"Evolución y características sedimentológicas de las facies fluviales basales del Buntsandstein de Olesa de Montserrat (Provincia de Barcelona).","authors":"P. Monzón, M. M. Carpio","doi":"10.5209/REV_CGIB.1977.V4.2891","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1977.V4.2891","url":null,"abstract":"","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"11 3","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"133169679","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 8
Facies aalenienses y bajocienses, con evidencias de emersión y carstificación, en el sector central de la Cuenca Ibérica. 伊比利亚盆地中部的aalenian和bajocian相，有出现和岩溶作用的证据。
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1990.V14.2637
S. Fernández-lópez
{"title":"Facies aalenienses y bajocienses, con evidencias de emersión y carstificación, en el sector central de la Cuenca Ibérica.","authors":"S. Fernández-lópez","doi":"10.5209/REV_CGIB.1990.V14.2637","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1990.V14.2637","url":null,"abstract":"Este trabajoforma parte de los proyectos de investigacion ID 452y 3394 subvencionodos \u0000por la C.A.I.C.Y.T y C.S.I.C","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"109 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"133462796","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 16
Análisis y distribución de facies del Cretácico inferior del Prebético en la provincia de Alicante 阿利坎特省下白垩纪前贝提科相的分析与分布
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1982.V8.2773
H. Wilke, J. A. Vera, M. García-hernández, A. López-garrido
{"title":"Análisis y distribución de facies del Cretácico inferior del Prebético en la provincia de Alicante","authors":"H. Wilke, J. A. Vera, M. García-hernández, A. López-garrido","doi":"10.5209/REV_CGIB.1982.V8.2773","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1982.V8.2773","url":null,"abstract":"Patrocinado por la C.A.I.C.Y.T., dentro del proyecto \"El Mesozoico de las Cordilleras Beticas\" \u0000desarrollado por el Departamento de Investigaciones Geologicas \u0000C.S.I.C. de Granada.","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"193 9","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"114095335","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 9
«Observations Micropaleontologiques sur le Malm á l'Ouest de Sezimbra (Portugal)» Sezimbra(葡萄牙)malma西部的微观古生物学观察
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1971.V2.2983
M. Ramalho
{"title":"«Observations Micropaleontologiques sur le Malm á l'Ouest de Sezimbra (Portugal)»","authors":"M. Ramalho","doi":"10.5209/REV_CGIB.1971.V2.2983","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1971.V2.2983","url":null,"abstract":"","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"22 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"117318744","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 2
Tectonism and vulcanicity of the Permocarboniferous Basin and Range Province of Western Europe. 西欧二叠石炭系盆地及山脉省的构造与火山活动。
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1977.V4.2874
V. Lorenz
{"title":"Tectonism and vulcanicity of the Permocarboniferous Basin and Range Province of Western Europe.","authors":"V. Lorenz","doi":"10.5209/REV_CGIB.1977.V4.2874","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1977.V4.2874","url":null,"abstract":"During the Carboniferousdic elongatedSouth EuropePlate was bounded by two fold beltswhich migratedaway from a centralcontinentalridge, pointing to two subductionzonesalong the NW and SE ma¿rginsof South Europe retreatingocean-wards.Due to releaseof abondantwater during subduetion, dehydrationand probablepartial melting of former oceaniccrust at the two subductionzones,one or severalupper mantle diapirs formed. Ríse of this hot upper mantle material causedwidespreadpartial melting in the lower crust of SouthEuropeandhigh temperature-lowpressuremetamorphism,and is believed to have reducedthe thickness and rigidity of the South Europe Plate considerably. Subductionof the Mid-Europeanoceancrust northwestof South Europe finally lcd to collision with North America-Europeand subduction of the Tethys oceancrust lcd to collision of South Europewith Africa in the southwest. Both collisions terminatedthe orogenicactivity at the sites of the fold bites. Approaching North Amcrica-EuropeandAfrica, South Europecollided with the irregulary rifted continental margins of the two adjacent plates. Enabledto do so by its reducedrigidity the South Europe Plate consequently deformed in orderto fit the irregularitiesof the adjacentcontinentalmargins. The originally presumablecollinearstructuresof South Europewere distorted and through rotations and translationsa number of subplatesformed separated from cach other by major wrench faults. The late Hercyniangeodynamic history of the various subplatesdevelopedalong similar paths. The hot uppcr mantle diapir causedregional uplift of the crust of South Europe,retreal of the seaand extensiveerosion.In additionlateral spreading of the diapir lcd lo regional crustal extensionand formation of intermontane graben-likebasins.Crustal spreadingwas initiated in the central continental ridge in uppermostVisean time xvhile simultaneouslyin the northwest and southeastcompressivestressregimeswere maintainedbecauseof the continued activity of the subductionzones. Shortly afterwards the firsí basaltic","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"168 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"114748710","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 1
Nuevos datos sobre la estratigrafía, paleontología y procedencia paleogeográfica del Triásico de las escamas del Corredor del Boyar (Cordillera Bética Occidental) 波雅尔走廊鳞片三叠纪地层学、古生物学和古地理起源新资料(西贝提山脉)
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1995.V19.2567
N. Porta, Ana Márquez-Aliaga, Agustín Martín-algarra
{"title":"Nuevos datos sobre la estratigrafía, paleontología y procedencia paleogeográfica del Triásico de las escamas del Corredor del Boyar (Cordillera Bética Occidental)","authors":"N. Porta, Ana Márquez-Aliaga, Agustín Martín-algarra","doi":"10.5209/REV_CGIB.1995.V19.2567","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1995.V19.2567","url":null,"abstract":"The Upper Triassic of the Boyar Corridor (External zones, Western Betic Cordillera) is constituted by a lower carbonate unit and an upper clayey-sandy unit. Both units provide Upper Carnian palynological associations. Besides, the lower unit contains associations of bivalves similar to those of the alpine «Raibler Schichten». These lithostratigraphic units were deposited in very shallow marine (subtidal) and coastal plain environments (peritidal in a broad sense), that constituted the internal areas of a marine shelf that evolved from mainly carbonatic to siliciclastic along the Uper Triassic. The Triassic of the Boyar Corridor is thinner than the typical Median Subbetic Upper Triassic, but it contains much less clays and evaporites and more carbonate marine intercalations than the former. This fact as well as its tectonic position along the contact between the Median Subbetic and the Penibetie, allow to locate it in the palaeogeographic transition between both domains.","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"61 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"114830229","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 11
CARACTERíSTICAS CERAMICAS DE ALGUNAS ARCILLAS DEL CRETACICO INFERIOR DEL MAESTRAZGO MAESTRAZGO下白垩世某些粘土的陶瓷特征
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1982.V8.2792
J. B. Cuairan, J. Enrique
{"title":"CARACTERíSTICAS CERAMICAS DE ALGUNAS ARCILLAS DEL CRETACICO INFERIOR DEL MAESTRAZGO","authors":"J. B. Cuairan, J. Enrique","doi":"10.5209/REV_CGIB.1982.V8.2792","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1982.V8.2792","url":null,"abstract":"","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"1 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"115130119","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 3
首页 上一页 下一页 尾页
0
×
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
请完成安全验证×
相关产品
×
本文献相关产品
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 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号：604180095
Book学术官方微信
小红书