Titlebook: Geological maps: An Introduction; Alex Maltman Book 1990 Alex Maltman 1990 document.information.remote sensing.time

有罪

栖息地

艰苦地移动

Unconformities,g directly upon vertical beds, became the first to perceive the long time interval implied by this kind of junction. The underlying material had to have been buried, lithified, rotated, and uplifted before the red sandstones were deposited on it.

monochromatic

More on faults: contraction (thrust), extension, and strike-slip faults,e found. It is a rare map which does not show a fault of one kind or another, but this chapter is mainly concerned with those areas of the earth where faults are numerous and dominated by a particular type.

尽管

Igneous and metamorphic rocks; mineral deposits,ch unit tends to have an overall tabular shape, being bounded at its top and bottom by roughly parallel surfaces, which enables three dimensional interpretations from maps and sections. We have, however, to be more cautious with non-sedimentary materials, for their shape can be much less regular. It is with these that this chapter is concerned.

Calculus

Astigmatism

cogent

茁壮成长

Die trigonometrische Parametrisierung,e patterns on the map record the relationships between the rocks, from which the geologist can deduce much about their arrangement underground and about their geological history. This book is aimed at helping you develop these interpretive skills.

Condescending