Geocol - Ramos (2010)
Authored by Spikings Hubach
Science
University
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10 questions
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1.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
El basamento de los Andes, desde Colombia hasta Argentina presenta edades magmáticas y metamórficas de:
1000-1200 Ma
900-1000 Ma
950-1300 Ma
650-800 Ma
2.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
El ensamblaje de Rodinia se produjo durante el Periodo:
Ediacariano
Fortuniano
Noriano
Steniano
3.
MULTIPLE CHOICE QUESTION
1 min • 1 pt
Diga la antiguedad en Ma (Ramos 2010) y el nombre de la unidad geocronológica (Era) correspondiente a la Orogenia Grenvilliana. Indique si dicho evento corresponde a subdcción o a choque de placas continentales. Diga los nombres de las placas
1200-1000Ma MesoProt. Choque de placas: Laurentia y Amazonia, quizá Báltica
1200-1000Ma PaleoProt. Choque de Báltica y Amazonia
1200-1000Ma MesoProt. Subducción: Laurentia y Amazonia
1200-1000Ma NeoProt. Subducción: Laurentia y Amazonia, quizás Baltica
4.
MULTIPLE CHOICE QUESTION
1 min • 1 pt
El Terreno Oaxaquia:
Cree que es un bloque adozdo a la margen de suramérica
Piensa que ese terreno de deslizó de norte a sur hacia Perú
Cree que ese terreno se deslizó por la zona de subduccion desde Perú a Mex.
Cree que simplemente es corteza oceánica adozada el margen continental
5.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
¿Cuándo se presenta silencio tectónico al W de Suramérica?
1000-540Ma
950-650Ma
1200-1000Ma
1000-800Ma
6.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
El silencio tectónico ocurre en respuesta a que:
Las particulas de circón fueron reseteadas por un evento termal
El histograma de edades no muestra partículas para este intervalo
El borde continental es un margen pasivo
El borde continental es un margen transformante
7.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
Durante la Orogenia Panafricana, los cinturones móviles son de tipo:
Andino (corteza superficial-juvenil) y Polimetamórfico (corteza antigua)
Polimetamórfico (corteza superficial-juvenil) y Andino (corteza antigua)
Colisionales
Ofiolíticos
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