CARACTERIZACIÓN DE LOS MATERIALES SEDIMENTARIOS INCONSOLIDADOS COSTEROS Y ALUVIALES ACTUALES EN LA REGIÓN DE PARRITA, PACÍFICO CENTRAL DE COSTA RICA
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| المؤلف: | |
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| التنسيق: | artículo original |
| الحالة: | Versión publicada |
| تاريخ النشر: | 2011 |
| الوصف: | Two different sedimentary environments (alluvial and coastal setting) have been recognized inthe Parrita area. The continental environment is represented by alluvial facies (alluvial plains, active meandricchannels, active braided river channels, and paleomeandric channel facies), and small lacustrine deposits. Thecoastal environment is conformed by beach, sand bars, and estuarine facies. The beach facies are formed by theassign of the littoral currents (NW-SE), which carry out the sediment from the adjacent coast and may be fromthe inner platform. The sand bars and estuarine facies constitute a bar barrier system. This system is formed bya sequence of sand bars and swamps, which are colonized by "mangle" vegetation. The granulometriccharacteristics of sediments (mean, mode, sorting, skewness, kurtosis) typify every sedimentary facies. |
| البلد: | Portal de Revistas UCR |
| المؤسسة: | Universidad de Costa Rica |
| Repositorio: | Portal de Revistas UCR |
| اللغة: | Español |
| OAI Identifier: | oai:portal.ucr.ac.cr:article/7775 |
| الوصول للمادة أونلاين: | https://revistas.ucr.ac.cr/index.php/geologica/article/view/7775 |
| كلمة مفتاحية: | planos aluviales ambientes costeros características granulométricas depósitos lacustres estuarios parrita costa rica canales meándricos canales trenzados alluvial plains coastal setting granulometric characteristics lacustrine deposits estuary meandric channels braided channels |