-
Gelasian is
defined magnetostratigraphically as the base of the
Matuyama (C2r)
chronozone (at the Gauss-Matuyama
magnetostratigraphic boundary), isotopic...
- but
different kinds of
stratigraphic units known collectively as
magnetostratigraphic units (magnetozones). The
magnetic property most
useful in stratigraphic...
-
equivalent to a
chronostratigraphic chronozone.
These correlate with
magnetostratigraphic, lithostratigraphic, or
biostratigraphic units as they are based...
- The
lower boundary of the
Pleistocene Series is
formally defined magnetostratigraphically as the base of the
Matuyama (C2r) chronozone,
isotopic stage 103...
- that
occurred 2.58 Ma and its
correspondence to the Gauss-Matuyama
magnetostratigraphic boundary. In 2006 ICS and
INQUA reached a
compromise that made Quaternary...
- ; Kent,
Dennis V.; Boersma, Anne; Rakic-El Bied,
Kruna (1994). "
Magnetostratigraphic, Biostratigraphic, and
Stable Isotope Stratigraphy of an
Upper Miocene...
-
Following statistical analysis, the
results are used to
generate a
local magnetostratigraphic column that can then be
compared against the
Global Magnetic Polarity...
-
Andrew P.; Norris, R. D. (20
November 2010). "New biostratigraphic,
magnetostratigraphic and
isotopic insights into the
Middle Eocene Climatic Optimum in...
- and
eastern Pacific Ocean and
comparison with
biostratigraphic and
magnetostratigraphic age data". GSA Bulletin. 98 (2): 207–223. doi:10...
- of the
Quaternary System and the
Pleistocene Series) is
defined magnetostratigraphically as the base of the
Matuyama (C2r)
chronozone (at the Gauss-Matuyama...
