- 1016/S0301-9268(02)00167-5. Fairbridge,
Rhodes W.;
Finkl Jr.,
Charles W. (1980). "
Cratonic erosion unconformities and peneplains". The
Journal of Geology. 88 (1):...
- than
twice the
typical 100 km (60 mi)
thickness of
mature oceanic or non-
cratonic,
continental lithosphere. At that depth,
craton roots extend into the asthenosphere...
- in the form of
North America,
although originally it also
included the
cratonic areas of
Greenland and the
Hebridean terrane in
northwest Scotland. During...
- A
cratonic sequence (also
known as megasequence,
Sloss sequence or su****quence) in
geology is a very large-scale
lithostratigraphic sequence in the rock...
- and
eastern part of the
continent and
represents one of Earth's
largest cratonic regions. The
Guiana Shield and
Central Brazil Shield (Guaporé Shield) constitute...
-
North America South America Zealandia Due to a
seeming lack of
Precambrian cratonic rocks, Zealandia's
status as a
geological continent has been
disputed by...
- Some of the
events ****ociated with the ****embly of
Columbia are: the
cratonic blocks in
South America and West
Africa were
welded by the 2.1–2.0 Ga Transamazonian...
-
Idealized cross-section of Earth's
lithosphere (Abbreviations: cb=
cratonic basin, LIP=large
igneous province, MOR=mid-ocean ridge)...
-
Gneiss in the
Northwest Territories on the
Canadian Shield, and on
other cratonic regions such as
those on the
Fennoscandian Shield. Some
zircon with age...
-
Krishna Godavari Basin is a peri-
cratonic p****ive
margin basin in India. It is
spread across more than 50,000
square kilometres in the
Krishna River and...
