SciELO - Scientific Electronic Library Online

 
 número56Un estudio explorativo de los Sistemas Convectivos de Mesoescala de México índice de autoresíndice de materiabúsqueda de artículos
Home Pagelista alfabética de revistas  

Servicios Personalizados

Revista

Articulo

Indicadores

Links relacionados

  • No hay artículos similaresSimilares en SciELO

Compartir


Investigaciones geográficas

versión On-line ISSN 2448-7279versión impresa ISSN 0188-4611

Resumen

HERNANDEZ SANTANA, José Ramón  y  ORTIZ PEREZ, Mario Arturo. Morphostructural analysis of the hydrographic basins of Sabana and Papagayo rivers (middle-lower third), Guerrero State, Mexico. Invest. Geog [online]. 2005, n.56, pp.7-25. ISSN 2448-7279.

This study presents the morphostructural patterns of the lower parts of the Papagayo and Sabana river basins, formed during the neotectonic (N-Q) stage. The structural framework consists of positive and negative blocks, which inherited their internal structure from different lithologic complexes and from older phases of tectonic deformation. The morphostructures can be distinguished, among others: massive, on granite basement; blocks on folds and monoclinals, on terrigenous and calcareous rocks; chaotic, on gravitational deposits; unconsolidated, on young deposits; and others types. Neotectonics has acted differentially, determining diverse faulting styles. The designs of granitic and metamorphic foliations are superimposed on those styles, as a tectonically passive expression of lithology. Finally, the study found 32 types of morphostructures, associated in several geotectonic communities of blocks, among others: irregular system of blocks; system of stepped triangular horst, deformed by transcurrent faults; isometric system of stepped blocks; alternate asymmetral system of horst and graben; system of stepped blocks on circular and annular structures; and others.

Palabras llave : Morphostructure; structural-geomorphological cartography.

        · resumen en Español     · texto en Español     · Español ( pdf )

 

Creative Commons License Todo el contenido de esta revista, excepto dónde está identificado, está bajo una Licencia Creative Commons