- The
Kimban orogeny, also
termed the
Strangways orogeny,
affected the
Gawler Craton in what is now
Australia between 1.73 and 1.69
billion years ago in...
- system.
Columbia forms as the
second undisputed earliest supercontinent.
Kimban Orogeny in
Australian continent ends.
Yapungku Orogeny on
Yilgarn craton...
-
Barramundi orogeny –
MacArthur Basin,
northern Australia, (c. 1890–1850 Ma)
Kimban orogeny –
Gawler Craton,
South Australia, (c. 1845–1700 Ma)
Cornian orogeny...
-
continental terrain. The
Mawson Continent seems to have
formed during the
Kimban orogeny of
around 1730–1690 Ma when the Gawler–Adélie
Craton combined with...
-
Hutchison Group (ca. 1900–1845 Ma)
prior to its
deformation during the
Kimban orogeny (ca. 1845–1710 Ma). On
northeastern Eyre Peninsula, the
Cleve Subdomain...
- and 1.55
billion years ago
which reworked rocks metamorphosed during the
Kimban orogeny. List of
orogenies Geology of
Australia Payne, J.L. and co-authors...
-
terrain was
accreted to the Gawler–Adélie
Craton during the 1730–1690 Ma
Kimban–Nimrod Orogeny, with a
suture zone that may be at or near the
location of...
- Montana:
collision between Hearne and
Wyoming cratons c. 1,765 Ma – As
Kimban Orogeny in
Australian continent slows,
Yapungku Orogeny (1.765 Gyr) begins...
-
belonging to the
Lincoln Complex of
granitic rocks intruded during the
Kimban Orogeny, 1600 to 1800 Ma." As of 1982, it was
reported that the island/reef...
