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The Ponta Grossa Arch: A proposal for ts configuration and evolution from the interpretation of remote sensing dataVisual analysis of MSS imagery was used to construct a map of dikes in a wide area of the Ponta Grossa Arch both in the Parana Basin and its basement. Analysis of the map by photographic methods defined the zone of highest density of the dikes, and some aspects of the longitudinal and transverse heterogeneities, as well as localized the apex of the Arch. Borders of the Arch were also suggested. Field investigations confirmed the position of the apex of the flexure on Palezoic sediments and pre-lava Mesozoic sediments. Controversial aspects of the relative absence of dikes in certain units or lithologies and the composition of intrusions surrounding the city of Castro were observed. The apparent synchronism between the activity of the Parana Basin and the Arch is discussed as well as the frequent inverse characteristics of vertical movements. The similarity of rocks in Brazil and Africa is also considered.
Document ID
19830019049
Acquisition Source
Legacy CDMS
Document Type
Thesis/Dissertation
Authors
Parada, N. D. J.
(Instituto de Pesquisas Espaciais Sao Jose dos Campos, Brazil)
Dealmeida, T. I. R.
(Instituto de Pesquisas Espaciais Sao Jose dos Campos, Brazil)
Date Acquired
September 4, 2013
Publication Date
January 1, 1983
Subject Category
Earth Resources And Remote Sensing
Report/Patent Number
INPE-2624-TDL/108
NASA-CR-172671
E83-10345
NAS 1.26:172671
Accession Number
83N27320
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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