• Nenhum resultado encontrado

Review of Survey activities 2004: Greenstone belts in the central Godthåbsfjord region, southern West Greenland

N/A
N/A
Protected

Academic year: 2017

Share "Review of Survey activities 2004: Greenstone belts in the central Godthåbsfjord region, southern West Greenland"

Copied!
4
0
0

Texto

Loading

Imagem

Fig. 1. Overview map of the central Godt- Godt-håbsfjord region – the focus of mapping and sampling in 2004 – and distribution of  green-stone belts (dominantly comprised of  amphi-bolite)
Fig. 3. Angular volcanic clasts in amphibolite of intermediate composi- composi-tion, Qussuk peninsula.
Fig. 4. East-closing synform in the footwall of the Storø shear zone, on the south-western slopes of Qingaaq mountain on Storø (see Fig

Referências

Documentos relacionados

The fourth generation of sinkholes is connected with the older Đulin ponor-Medvedica cave system and collects the water which appears deeper in the cave as permanent

The limestone caves in South Korea include a variety of speleothems such as soda straw, stalactite, stalagmite, column, curtain (and bacon sheet), cave coral,

financeiras, como ainda por se não ter chegado a concluo entendimento quanto à demolição a Igreja de S. Bento da Ave-Maria, os trabalhos haviam entrado numa fase

In the central portion of the study area, we have defined the occurrence of two alkali-feldspar granite bodies (Serra Alkali Feldspar Granite, Guimarães et al.. Figure 8 -

The transition zone between the Pernambuco-Alagoas Domain and the Sergipano Belt (Borborema Province, NE Brazil): Geochronological constraints on the ages of deposition,

Geological mapping using remote sensing data: a comparison of five machine learning algorithms, their response to variations in the spatial distribution of training data and the

The HAND model, which in turn, defines the terrain height thresholds that fall into the susceptibility classes, was cut from the susceptible relief vectors, i.e., areas of the

Os modelos desenvolvidos por Kable & Jeffcry (19RO), Skilakakis (1981) c Milgroom & Fry (19RR), ('onfirmam o resultado obtido, visto que, quanto maior a cfiráda do