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El Cretácico del Macizo de Caroch (provincias de Valencia y Albacete) 卡罗赫山脉的白垩纪(巴伦西亚和阿尔巴塞特省)
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1979.V5.2871
A. Meléndez
{"title":"El Cretácico del Macizo de Caroch (provincias de Valencia y Albacete)","authors":"A. Meléndez","doi":"10.5209/REV_CGIB.1979.V5.2871","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1979.V5.2871","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":"130748545","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
Cyclic lagoonal sedimentation of the Oxfordian/ Kimmeridgian within the Sierra del Madero, Northwestern Iberian Range, Soria province 索里亚省伊比利亚山脉西北部马德罗山脉内牛津/基默里吉亚盆地的旋回泻湖沉积
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1990.V14.2643
S. Wilde, H. Mensink, D. Mertmann
{"title":"Cyclic lagoonal sedimentation of the Oxfordian/ Kimmeridgian within the Sierra del Madero, Northwestern Iberian Range, Soria province","authors":"S. Wilde, H. Mensink, D. Mertmann","doi":"10.5209/REV_CGIB.1990.V14.2643","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1990.V14.2643","url":null,"abstract":"During the Oxfordian ant! Lower Kimmeridgian a lagoon developped in the area of the westemn Madero. Therc a cyclic carbonate sedimentation of shallow subtidal to intertidal cnvironmcnt took place. The alternation repmesents a number of transgressive ant! regressive facies variations. Oolitic bars and clastie delta sediments from the Ebro Massif and dic Soi-iaAteca-High isolated the lagoon from the open marine shclfsituated southeast of Olvega. The age determinations are based upon foraminifera ant! algae.","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":"130918125","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
Estratigrafía del Jurásico en Asturias 阿斯图里亚斯侏罗纪地层学
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1974.V3.N1.2936
L. C. S. Vega
{"title":"Estratigrafía del Jurásico en Asturias","authors":"L. C. S. Vega","doi":"10.5209/REV_CGIB.1974.V3.N1.2936","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1974.V3.N1.2936","url":null,"abstract":"","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"2 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":"133503126","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: 49
Interpretación paleoambiental de depósitos siliciclásticos en el sector de Esquivias (Cuenca de Madrid) Esquivias区硅质碎屑沉积古环境解释(马德里盆地)
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1997.V22.2516
J. Casas, M. Pozo
{"title":"Interpretación paleoambiental de depósitos siliciclásticos en el sector de Esquivias (Cuenca de Madrid)","authors":"J. Casas, M. Pozo","doi":"10.5209/REV_CGIB.1997.V22.2516","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1997.V22.2516","url":null,"abstract":"The occurrence of kerolite-stevensite bearing lithofacies in Neogene Madrid Basin has special outstanding in the Esquivias deposit (Toledo>. In tliis zone Mg elays are bounded at top and bottom by two detrital units. In tliis paper the mineralogical association and sedimentological features of sandy facies related to lower detrital unit (arenas 1), magnesie unit (arenas 2) and upper detrital unit (arenas 3> has been studied. Granulometrie results are: high centile, median values ranging between 0.12 and 0.20 mm. (80ixm % in arenas 2) and good sorting with ranging between 1.58 and 2.07 (up to 4.5 in arenas 2). The sandy facies mineralogy aJways shows feldspars (Ca-Na>K> predominance over quartz and variable content in mica. Heavy mineral assemblages mainly are made up of: biotite, zircon, apatite, tourmaline, garnet and andalusite. Olten these minerals, even apatites, show euhedrail grains, sometimes with unweathered surfaces. Siliciclastie alluvial sedimentation in saline-alkaline lacustrine environment and semiarid climatie conditions are inferred.","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"36 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":"133581233","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
La transgresión del Cretácico superior en el sector de Atienza-Sigüenza (Guadalajara, Cordillera Ibérica) y el significado de la fauna ammonitífera. 上白垩纪海带atienza - siguenza(瓜达拉哈拉，科迪勒拉伊比利亚)和两栖动物群的意义。
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1982.V8.2759
J. Wiedmann, M. Segura
{"title":"La transgresión del Cretácico superior en el sector de Atienza-Sigüenza (Guadalajara, Cordillera Ibérica) y el significado de la fauna ammonitífera.","authors":"J. Wiedmann, M. Segura","doi":"10.5209/REV_CGIB.1982.V8.2759","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1982.V8.2759","url":null,"abstract":"","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"68 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":"128826931","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
Litoestratigrafía del Cretácico superior del Altiplano de Jumilla-Yecla (Zona Prebética.) Jumilla-Yecla高原上白垩纪岩石地层学(前betica带)
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1994.V18.2576
J. Martín‑Chivelet
{"title":"Litoestratigrafía del Cretácico superior del Altiplano de Jumilla-Yecla (Zona Prebética.)","authors":"J. Martín‑Chivelet","doi":"10.5209/REV_CGIB.1994.V18.2576","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1994.V18.2576","url":null,"abstract":"El CretAEcicosuperior del Altiplano de Jumilla - Vecla (SE de Espaaea) estAEconstituido por potentes series carbonAEticaso mixtas desarrolladas en las plataformas prebOticas.Su estudio permite proponer un patr n litoestratigrAEficoglobalmente nuevo, constituido por dieciocho unidades (quince formaciones y tres miembros). Ese patr n constituye una base para las correlaciones interregionales de las plataformas cretAEcicasdel SE de Espaaea.Dichas unidades se han enmarcado en seis megaseduencias de dep sito con edades comprendidas entre el Albiense superior y el Maastricbtiense superior. stas perfilan una evoluci n de las plataformas prebOticasfuertemente controlada por la tect nica sinsedimentaria y, en menor proporci n, por el eustatismo.","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"64 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":"128864737","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: 26
Itineraire géologique á travers le Crétacé moyen des chames Vascogotiques et Celtibériques. ( Espagne du Nord). Appendice B. Le calcaire de Caniego: temoin d'une montée du diapir de Valle de Mena (prov.Burgos, Espagne) dans l'Albien supérier 穿越中白垩纪瓦斯科哥特和凯尔特盆地的地质路线。(西班牙北部)。附录B. Caniego石灰石:Valle de Mena diapir上升的证据(prov。西班牙布尔戈斯)在阿尔比亚superior
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1979.V5.2857
R. Schroeder
{"title":"Itineraire géologique á travers le Crétacé moyen des chames Vascogotiques et Celtibériques. ( Espagne du Nord). Appendice B. Le calcaire de Caniego: temoin d'une montée du diapir de Valle de Mena (prov.Burgos, Espagne) dans l'Albien supérier","authors":"R. Schroeder","doi":"10.5209/REV_CGIB.1979.V5.2857","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1979.V5.2857","url":null,"abstract":"","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"5 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":"127865024","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
Análisis secuencial durante el intervalo Barremiense-Aptiense en la Cubeta de Oliete Oliete桶中barremien - aptiense间隔的顺序分析
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1993.V17.2599
Emmanuelle Vennin, A. Soria, Alain Préat, A. Meléndez
{"title":"Análisis secuencial durante el intervalo Barremiense-Aptiense en la Cubeta de Oliete","authors":"Emmanuelle Vennin, A. Soria, Alain Préat, A. Meléndez","doi":"10.5209/REV_CGIB.1993.V17.2599","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1993.V17.2599","url":null,"abstract":"The lower Cretaceous (Upper Barremian-Upper Aptian) marine sediments of the Oliete basin (NE Spain) were traditionnally grouped in the Alacon limestone Formation, Forcali man Formation and Oliete limestone Formation. Ihe identification of several discontinuities of regional extend allows us to establish ibree dispositional sequences for this sedimentary record which are tentatively correlated with the sequences Late Barremian (Kl.'?), Early Aptian (KI.8) and Late Aptian (K1.9) defined in the Maestrazgo adyacent basin. Further subdivision of these sequences in system tracts was based on extensive facies and microfacies analysis. In the lower sequence lowstand, transgressive and highstand system tract were identified while only transgressive and highstand systems 1 act were recognized for the upper two sequences. Key-Words: Early Cretaceous, Barremian, Aptian, Oliete sub-basin, Ramp, Sequence Stratigraphy.","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"20 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":"131298769","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: 6
Facies carbonato-evaporíticas del Trías Superior y tránsito al Lías en el Levante español: nuevas precisiones estratigráficas. 西班牙莱万特上三叠纪碳酸盐-蒸发岩相及向泥岩过渡:新的地层精度。
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1996.V20.2550
N. Porta, F. Cabo, A. Pérez-lópez
{"title":"Facies carbonato-evaporíticas del Trías Superior y tránsito al Lías en el Levante español: nuevas precisiones estratigráficas.","authors":"N. Porta, F. Cabo, A. Pérez-lópez","doi":"10.5209/REV_CGIB.1996.V20.2550","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1996.V20.2550","url":null,"abstract":"En este trabajo se abordan diversos aspectos problematicos dcl transito del Triasico Superior al Liasico en la zona de Levante, sobre todo con relacion a la litoestratigrafia y a la datacion palinologica. A partir de varios cortes parciales de materiales triasicos del Levante seleccionados en el Prebetico oriental y dominio Iberico mas meridional (Jumilla, Ontur, Almansa, Cofrentes, Domeno), y tomando como referencia la identificacion de la unidad K5 del Keuper (Formacion Yesos de Ayora), se ha establecido una estratigrafia de los distintos conjuntos litologicos del transito Trias-Lias: Unidad K5, Formacion Zamoranos/Formacion Imon, Anhidrita de Carcelen (Fm. Cortes de Tajuna). Los escasos datos palmologicos existentes sugieren que estos conjuntos litologicos pertenecen al Noriense (incluido el Retiense), al menos en parte.","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"134 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":"124163873","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: 15
Perspectiva de la minería del carbón en Teruel 特鲁埃尔煤矿开采的前景
Journal of iberian geology: an international publication of earth sciences Pub Date : 1900-01-01 DOI: 10.5209/REV_CGIB.1993.V17.2587
M. A. Albéniz
{"title":"Perspectiva de la minería del carbón en Teruel","authors":"M. A. Albéniz","doi":"10.5209/REV_CGIB.1993.V17.2587","DOIUrl":"https://doi.org/10.5209/REV_CGIB.1993.V17.2587","url":null,"abstract":"En el conjunto de las distintas formaciones pertenecientes al periodo Mesozoico, en el ambito de la Cordillera Iberica, es la de Escucha la mas relevante desde el punto de vista de su aprovechamiento industrial, al contener en sus tres miembros capas de carbon susceptibles de explotacion para su aprovechamiento en el campo de la produccion termoelectrica. Las dificultades inherentes a la explotacion en mineria subterranea se obvian con los metodos de explotacion a cielo abierto, altamente mecanizados y selectivos que posibilitan una mineria de grandes volumenes, por lo que importantes trabajos de restauracion deben ser acometidos. Por ultimo la innovacion tecnologica en el campo de la combustion en lecho fluido y la gasificacion subterranea del carbon, permitiran un aprovechamiento exhaustivo de las reservas de la Cuenca Minera de Ternel.","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"192 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":"124328356","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
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