Zobrazeno 1 - 7
of 7
pro vyhledávání: '"J. Pablo Rodríguez-Aranda"'
Publikováno v:
Geogaceta, Vol 70 (2021)
La laguna de Caballo Alba (Segovia) es un pequeño lago efímero hiperalcalino del Humedal Coca-Olmedo de salmueras clorurado-sódicas, cuyo sustrato y área de drenaje están formados por rocas margosas miocenas y retazos de terrazas cuaternarias. E
Externí odkaz:
https://doaj.org/article/b7b6e819e69f43dd992fd7a7cc872a1f
Publikováno v:
E-Prints Complutense. Archivo Institucional de la UCM
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This work provides the first evidence of seismites within Miocene gypsum microbialites deposited in inland lakes. Seismites are observed on good quality outcrops in two separated successions of the Madrid and Duero basins (central Spain) that are sit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7dd88a9f09514105e35585b51a120700
https://doi.org/10.1016/j.sedgeo.2022.106219
https://doi.org/10.1016/j.sedgeo.2022.106219
Autor:
José-Pedro Calvo, J. Pablo Rodríguez-Aranda, Raimundo Outerelo, M. Esther Sanz-Montero, M. Ángeles García del Cura, Concepción Ornosa
Publikováno v:
Terra Nova. 25:465-471
Shoreline gypsiferous sediments of an inland lake in central Spain furnishes valuable insight into reconstructions of early sedimentary changes related to shore fly–microbial mat interactions in fossil gypsum precipitating saline lake systems. The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::613901e66adce8370aed653f6de736b2
https://doi.org/10.1111/ter.12058
https://doi.org/10.1111/ter.12058
Publikováno v:
Sedimentary Geology. 222:138-148
This paper provides an ancient analogue for biologically mediated celestite and barite formation in dolomite precipitating microbial mats developed in lacustrine environments during the Miocene. Barite and celestite occurrences were studied in three
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::456415fb72df02ec8bd8bc66f6a6d4d4
https://doi.org/10.1016/j.sedgeo.2009.05.009
https://doi.org/10.1016/j.sedgeo.2009.05.009
Publikováno v:
Geological Magazine. 146:527-539
The Miocene dolomite-chert microbialites studied here offer a complete record of the geochemical cycles of silicate weathering and the subsequent formation of secondary products. The microbialites were formed in lacustrine systems during the Miocene
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::366de75c4deeb12bf43149773691f067
https://doi.org/10.1017/s0016756808005906
https://doi.org/10.1017/s0016756808005906
Publikováno v:
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
E-Prints Complutense. Archivo Institucional de la UCM
instname
Universidad Complutense de Madrid
E-Prints Complutense. Archivo Institucional de la UCM
instname
Based on petrographic, mineralogical, isotope, and facies assemblage analysis, a microbial origin is established for the formation of dolomite associated with gypsum in Miocene evaporite lake deposits of the Madrid Basin, central Spain. In these depo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::810966f9b5a0db95ba81fa321910dbce
https://eprints.ucm.es/id/eprint/58485/1/1257-1.pdf
https://eprints.ucm.es/id/eprint/58485/1/1257-1.pdf
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