19.07.2013 Views

PROJETO RADAM

PROJETO RADAM

PROJETO RADAM

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

ABSTRACT<br />

Results of regional geological mapping using radar imagery at 1:250.000 and<br />

1:1.000.000 scales are presented.<br />

The area of work corresponds to about 192.290sq. km., between longitudes<br />

40° 30' to 48° 00' west, and latitude 04° 00' south to the littoral. It<br />

encompasses the coastal parts of the Maranhao and Piaui States, and portions<br />

of the states of Para and Ceara. Geologically it corresponds to the northern<br />

part of the Piaui—Maranhao Sedimentary Basin, and the coastal areas in<br />

which the Barreirinhas and Sao Luis basins are located.<br />

The total area actually mapped comprises 780.000sq. km., covering all of the<br />

sedimentary basin and adjacent Precambrian terrains. However, for uniformity<br />

purposes, the global area was divided into three blocks corresponding ,<br />

likewise, to three different reports.<br />

The objectives of the work were twofold. First, coincident with that of<br />

<strong>RADAM</strong> PROJECT itself, to furnish, in a short period of time, a<br />

comprehensive panoramic sight of the most important geological aspects of<br />

extensive regions of north and northeast Brazil. Secondly, to verify the<br />

degree of detail that could be obtained with radar imagery, since the area<br />

had already been mapped with the use of other sensors.<br />

Initially, intention was to use data of previous work and merely transpose<br />

the information to the radar imagery. However, the complete failure of this<br />

procedure led to direct field investigation to determine the correspondence<br />

of imagery — geologic features. Based on this, preliminary interpretations<br />

were made, followed by field checking and compilation of the final maps.<br />

The area presents two assemblages of rocks quite distinct. The first is<br />

represented by Undivided Precambrian granitic and metamorphic rocks<br />

making up the Caraiba, Gurupi and Jaibaras groups. The second assemblage<br />

is comprised by sedimentary rocks ranging from Lower Paleozoic (Silurian)<br />

to Quaternary. Paleozoic formations are restricted to the northeastern<br />

margin of the basin, whereas about 80% of the region is covered by the<br />

Itapecuru (Cretaceous) and Barreiras (Tertiary) formations.<br />

I/7

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!