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Honduras Geology March, 1997, Edition 1.3

SAN FRANCISCO DE BECERRA, HONDURAS 1:50,000

Age/Edad Unit/ Unidad Descripción Description
Cenozoico Cuaternario Qal Aluvium - generally sands, gravels, and occassional pebbles of schist, standstone, or quartz.
Qt Terraces - stratified levels of floodplain deposits of predominantly sands, gravels and pebbles.
Terciario Tv Volcanics - crystal lithic breccias, lithic airfall tuffs, and densely welded pyroclastics.
Mesozoico Cretacico Grupo Valle de Angeles Valle de Angeles Group
Kva Redbed siliclastic strata primarily a quartz pebble conglomerate; some sandstone and schist clasts present, as well as large fossiliferous limestone pebbles. Cement is hematite and silica.
Jurasico Grupo Honduras Honduras Group
Jaf Agua Fria Formation - Fine grain, thin bedded tan sandstone with interbedded dark shales, dark shales with interbedded sandstones, and massive sandstones; quartz veining common; deformed metasediments and quartzites are also common.
Paleozoico Esquisto Cacaguapa Cacaguapa Schist
csp Primarily phyllitic schists, graphic and sericitic schists are also present; thick quartz veins along foliation is common; occassional large (1 cm) pyrite clasts present; large bodies of quartzite are rare.
Rocas Instrusivas Intrusive Rocks
i The metagranite consists of altered biotite, quartz, and feldspar; quartz veining is present.
i2 The diorite contains large phenocrysts of hornblende in addition to the feldspar matrix; quartz veining is present.

Fuente/Source: Michael J. Kozuch, 1989, Geology of the San Francisco de Becerra, Honduras, Central America unpublished report, Instituto Geografico Nacional, Tegucigalpa, Honduras


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