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Localización y estudio de un afloramiento básico efusivo en la Sierra de la Paramera-Avila (Sistema Central español) Sierra de la Paramera-Avila(西班牙中央系统)基本喷流露头的定位与研究
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1981.V7.2830
F. Calvo, A. G. Ubanell
{"title":"Localización y estudio de un afloramiento básico efusivo en la Sierra de la Paramera-Avila (Sistema Central español)","authors":"F. Calvo, A. G. Ubanell","doi":"10.5209/REV_CGIB.1981.V7.2830","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1981.V7.2830","url":null,"abstract":"By first time> in the sierra de La Paramera (Central Spanish System) one efusive basics rocks outcropping are pointed out. The geological and geophisical investigation have permitted the definition of his tectonic significance. This outcropping is a central vent of volcano of late --Hercynian times posible.","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"27 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":"121525691","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
Pérmico continental en España.
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1977.V4.2875
C. Virgili, Amparo Ramos, A. Sopeña, S. Costa
{"title":"Pérmico continental en España.","authors":"C. Virgili, Amparo Ramos, A. Sopeña, S. Costa","doi":"10.5209/REV_CGIB.1977.V4.2875","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1977.V4.2875","url":null,"abstract":"The present data show that the Spanish Permian is represented by the «Autunian» (Lower Rotliegendes) in a typical grey facies and redbeds similar to the «Saxonian» (Upper Rotliegendes). The Upper Permian has been found only in a very few points. In general it is made of detrital series, from clays to conglomerates; some volcanic levels are found. Tickness is very variable, up to 2.000 meters. Sedimentation takes place in continental basins, tectonically con troled 1w the tardihercynian pbases. Their caracteristics and problenis are similar to the ones of Western European Permian. 1.","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"24 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":"125224369","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
Ammonite biostratigraphy of the middle Jurassic sediments of Georgia = bioestratigrafía de las sucesiones del Jurásico Medio en Georgia 格鲁吉亚中侏罗世沉积物的菊石生物地层学= bioestratigrafía de las succesiones del Jurásico Medio en Georgia
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1998.V24.2481
T. Lominadze, M. Topchishvili, L. Tsereteli
{"title":"Ammonite biostratigraphy of the middle Jurassic sediments of Georgia = bioestratigrafía de las sucesiones del Jurásico Medio en Georgia","authors":"T. Lominadze, M. Topchishvili, L. Tsereteli","doi":"10.5209/REV_CGIB.1998.V24.2481","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1998.V24.2481","url":null,"abstract":"","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"64 7-8","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"131496389","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
Diferenciación de dos tramos en la formación Arenas de Utrillas según la respuesta en las diagrafías. 根据图中给出的答案，区分砂岩地层的两个部分。
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1993.V17.2601
E. Aracil
{"title":"Diferenciación de dos tramos en la formación Arenas de Utrillas según la respuesta en las diagrafías.","authors":"E. Aracil","doi":"10.5209/REV_CGIB.1993.V17.2601","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1993.V17.2601","url":null,"abstract":"En el presente trabajo se estudia el analisis secuencial de la Fm. Arenas de Utrillas en las diagrafias en algunos de los sondeos de petroleo de la Cordillera Iberica Meridional y del Prebetico. Estos sondeos son San Lorenzo de la Parrilla- 1, Belmontejo- lA, Gabaldon- 1 y Ledana- 1 (Sector Septentrional) y Carcelen-l, Socovos-2 y Rio Segura-GI (Sector Meridional). Tras el analisis de las diagrafias destacan cinco aspectos importantes: Notable diferencia de espesor de la Fm. Arenas de Utrillas entre el - Sector Norte (110 m) y el Sector Sur (35 m). Presencia de la Fm. Calizas, Margas y Areniscas de Sacaras en el Sector - Meridional, coincidiendo con una escasa potencia de la Fm. Arenas de Utrillas. Diferente tipo de electrosecuencias entre las partes inferior y superior de - la Fm. Arenas de Utrillas en el sector septentrional. Similitud de espesores y tendencia de las electrosecuencias entre Sacaras - y el tramo inferior de la Fm. Arenas de Utrillas. Similitud de espesores y electrosecuencias entre la parte superior de - Utrillas y la formacion del mismo nombre en el Sector Sur. Estos aspectos inducen a pensar que la parte inferior de Utrillas en la zo Cuadernos de Geologia Iberica, nfr 7, 311-324. Editorial Complutense, Madrid, 1993 E. Aracil 312 na estudiada de la Cordillera Iberica Meridional es el equivalente lateral de Sacaras en la Cordillera Iberica Suroccidental y el Prebetico.","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"8 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":"127674132","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
Coniferes et polen in situ du Buntsandstein de l'ile de Majorque(Baléares, Espagne) 马略卡岛（西班牙巴利阿里群岛）邦桑德斯坦原地的针叶树和多针叶树
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1996.V20.2549
C. Ramis, L. Grauvogel-Stamm
{"title":"Coniferes et polen in situ du Buntsandstein de l'ile de Majorque(Baléares, Espagne)","authors":"C. Ramis, L. Grauvogel-Stamm","doi":"10.5209/REV_CGIB.1996.V20.2549","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1996.V20.2549","url":null,"abstract":"The morphological study of two male eones from the upper part of the Buntsandstein (Estellencs unit) of the Majorca Island (Balearie Isles, Spain) shows that they belong to the conifer reproductive organ genus Willsiostrobus. The study of their pollen in situ indicates that they have to be attributed to two distinct species. One of them provided pollen grains corresponding to the sporae dispersae Voltziaceaesporites heteromorpha and could be referred to 1V rhomboidalis, a characteristie species of the GrOsAEVoltzia (Upper Buntsandstein) of northeastern France. The other one which was unknown before represents a new species, 1V hexasacciphorus. It is the reproductive organ which produced the hexasaccate pollen corresponding to the sporae dispersae known under two taxons Stellapollenites thiergartii and Hexasaccites muelleri, which also occurs in the GrOsAEVoltzia of the Vosges (France). The occurrence of this pollen type in the Estellenes unit indicates that the upper part of the Buntsandstein in the Majorca Island is Anisian, like the uppermost part of the Upper BuntConifOres et pollen in sita e/u Buntsandstein.. 231 sanstein in the northeastern France where it is represented by the GrOsAE Voltzia.","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"14 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":"134603395","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
Las discontinuidades mayores del Jurásico de las Zonas Externas de las Cordilleras Béticas: análisis e interpretación de los ciclos sedimentarios. 贝提斯山脉外带侏罗纪大不连续:沉积旋回的分析与解释。
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1989.V13.2648
P. A. Ruiz-ortiz, J. A. Vera, M. García-hernández, A. López-garrido, Agustín Martín-algarra, J. M. Molina
{"title":"Las discontinuidades mayores del Jurásico de las Zonas Externas de las Cordilleras Béticas: análisis e interpretación de los ciclos sedimentarios.","authors":"P. A. Ruiz-ortiz, J. A. Vera, M. García-hernández, A. López-garrido, Agustín Martín-algarra, J. M. Molina","doi":"10.5209/REV_CGIB.1989.V13.2648","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1989.V13.2648","url":null,"abstract":"El margen suriberico de las Zonas Externas de las Cordilleras Beticas evoluciono durante el Mesozoico como un margen transtensivo controlado por factores eustaticos, tectonicos, sedimentarios y climaticos. Las etapas de fracturacion, a lo largo del Jurasico, junto con los descensos eustaticos y los cambios en la velocidad de sedimentacion, dieron lugar a discontinuidades estratigraficas mayores, que han quedado desigualmente registradas en las series. Se reconocen cuatro discontinuidades mayores, cuya posicion en el espacio y tiempo se analiza. Las cuatro discontinuidades de orden mayor que se reconocen en el conjunto de la cuenca son: intracarixiense (controlada por la tectonica regional y mas secundariamente por el eustatismo), la del limite Lias-Dogger (esencialmente eustatica), la del limite Dogger-Malm (eustatica y tectonica) y la finijurasica (tectonica y eustatica). Estas discontinuidades separan megasecuencias cuya polaridad viene regulada por los factores antes citados. La historia jurasica corresponde a la de evolucion de un rift. en la que se reconocen las etapas prer~tt, sin 4/k y de expansion; el paso de una etapa a otra se realiza en la Zona Prebetica retrasado con respecto a la Zona Subbetica.","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"71 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":"133837144","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: 55
La marge Sud-Ouest d'Iberie pendant le Jurassique supérieur (Oxfordien-Kimmeridgien): essai de reconstruction geobiologique. 上侏罗纪伊比利亚西南边缘(牛津-金默里奇):地球生物学重建试验。
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1989.V13.2656
B. Marques, F. Olóriz
{"title":"La marge Sud-Ouest d'Iberie pendant le Jurassique supérieur (Oxfordien-Kimmeridgien): essai de reconstruction geobiologique.","authors":"B. Marques, F. Olóriz","doi":"10.5209/REV_CGIB.1989.V13.2656","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1989.V13.2656","url":null,"abstract":"","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"13 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":"130343956","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: 7
El Senoniense inferior del valle de Losa (Burgos) y sus microfaunas. 洛萨山谷(布尔戈斯)的下塞诺尼亚时期及其微动物群。
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1982.V8.2747
J. Lázaro
{"title":"El Senoniense inferior del valle de Losa (Burgos) y sus microfaunas.","authors":"J. Lázaro","doi":"10.5209/REV_CGIB.1982.V8.2747","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1982.V8.2747","url":null,"abstract":"Ihe calcareus-pelitie sequence of the Losa Valley (Basqne Cantabrie Basin) have about 1.300 m thick in the studied section. Micropaleontological studies have led to us to recognise the niost part of the Dicaririella concavata and 13. asymetrica Zones. The fossil communities of foraminifera and ostracods found in these rocks characterise, generally, a shelf deposition of circalittoral conditions towards the lower part of the sequence, upper lower Coniacian age, with abundant planktonic foraminifera. Ihese depositional conditions change to infralittoral ones in the upper part of the section, as it is shown by the planktonic foraminifera/foraminifera rate and the occurrence of ostracods with littoral affinities as the genera Xestoleberis, Schuieridea and Dordoniella. RESUMEN La secuencia de margas y margocalizas del Valle de Losa (Cuenca Vasco-Cantabrica) alcanza en el corte presentado hasta 1.300 m de potencia. El estudio micropaleontologico ha permitido reconocer la presencia, en su mayor parte, de las zonas de Dicarinetia concavata y de Dicarinella asymetrica. Las asociaciones de foraminiferos y ostracodos nos permiten caracterizar un ambiente de plataforma, en general con * Departamento de Paleontologia, Facultad de Ciencias, Universidad del Pais Vasco. 99 unas caracteristicas circalitorales hacia la base, Coniaciense inferior terminal, con abundancia de foraminiferos planctonicos. Condiciones que van cambiando a infralitorales con disminucion de la relacion de foraminiferos p]anctonicos a bentonicos y la presencia de ostracodos mas litorales como Xestoieberis, Schuleridea y Dordonietia, en los terminos superiores, bajo las calizas con Lacazina.","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"77 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":"114684235","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
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
Lower Permian to Miocene apparent polar wander path for Iberia and its bearings on kinematic evolution. 下二叠世至中新世伊比利亚的视极漂移路径及其与运动演化的关系。
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1988.V12.2660
J. Schott
{"title":"Lower Permian to Miocene apparent polar wander path for Iberia and its bearings on kinematic evolution.","authors":"J. Schott","doi":"10.5209/REV_CGIB.1988.V12.2660","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1988.V12.2660","url":null,"abstract":"A review of the reliable paleomagnetic poles for the Iberian plate is given in the range Permian to Miocene. After rejection of data belonging to displaced of deformed areas, or representing remagnetizations, 11 poles are selected. Using this data base, an Apparent Polar Wander Path (APW) is constructed. Two methods are used. The first one is a refined sliding window method. Ihe second one is the small circie fitting recently developped in APW modelling. This method is appropiate for the lower Perrnian-lower Jurassic track only. Finaily, the consistency of the APW with known kinematic models for Iberia is tested. There are, roughly speaking, two kinds of models describing the evolution of Iberia relative to Europe: single rotation models and left-lateral shift models. As a result, both models lead to statistically equivalent fits between the European and iberian APW’s, for the lower Permian-lower Jurassic track. Thus, it is clearly shown that the current lack of palcomagnetic data prevents us from giving close constraints to the kinernatic evolution of Iberia.","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"132 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":"114424703","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: 4
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