下寒武纪纳瓦鲁西洛斯组最西端:西班牙托莱多山中伊比利亚带潮汐沉积中的微生物岩

IF 0.8 4区 地球科学 Q3 GEOLOGY
S. Menéndez, M. Rodríguez-Martínez, E. Moreno-Eiris, A. Perejón
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引用次数: 0

摘要

在伊比利亚地块的伊比利亚中部地区,被解释为潮汐和浅海碳酸盐矿床的Los navalucilllos组包含了一个重要的古海藻动物组合。这里描述了靠近La Nava de Ricomalillo地区的地层最西端露头的两个新的特征暴露:(i) La Estrella,由于附近的深成杂岩,岩石受到接触变质作用的强烈影响;(ii) Finca - Higueruela演替,没有钙微生物-古藻黏结岩,尽管有明显的叠层石和肿瘤等微生物。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
El sector más occidental de la Formación de Los Navalucillos, Cámbrico inferior: microbialitas en yacimientos mareales de la Zona Centroibérica, Monte de Toledo, España
In the Central Iberian Zone of the Iberian Massif, the Los Navalucillos Formation, interpreted as tidal and shallow-marine carbonate deposits, contains a significant archaeocyathan faunal assemblage. Two new characteristic exposures are described here from the westernmost outcrops of the formation, close to La Nava de Ricomalillo area: (i) La Estrella, where the rocks are strongly affected by contact metamorphism due to the nearby plutonic complex; and (ii) the Finca Higueruela succession, without calcimicrobial-archaeocyathan boundstones, although different microbialites as stromatolites and oncolites are conspicuous.
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来源期刊
CiteScore
1.40
自引率
14.30%
发文量
6
审稿时长
>12 weeks
期刊介绍: Since 1945 Estudios Geologicos publishes original research works, as well as reviews, about any topic on Earth Sciences. Estudios Geologicos is published as one yearly volume, divided into two half-yearly issues. It is edited by the Spanish National Research Council (Consejo Superior de Investigaciones Científicas, CSIC) at the Instituto de Geociencias (CSIC-UCM). Estudios Geologicos provides free access to full-text articles through this electronic edition. Accepted articles appear online as "Forthcoming articles" as soon as the galley proofs have been approved by the authors and the Editor-in-Chief. No changes can be made after online publication.
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