- The
Qiangtang terrane was
located west of
Sibumasu and
contiguous with it.
Lower Permian layers in
Sibumasu contain glacial-marine
diamictites and Gondwanan...
- The Shan–Thai or
Sibumasu terrane was a
microcontinent which extended from
Lhasa (Tibet) West Yunnan, Myanmar, West Thailand, much of
Malaysia and Sumatra...
- terranes,
namely Indochina,
North China,
South China ,
Cimmerian terranes,
Sibumasu, Qiangtang, Lhasa, Afghanistan, Iran, Turkey – were
still attached to the...
-
western half is an
amalgamation of
continental terranes Sinoburmalaya or
Sibumasu.
These two
halves of
terranes were
separated by the Paleo-Tethys Ocean...
- species.
Other Asian terranes remained attached to Gondwana,
including Sibumasu (western Indochina), Tibet, and the rest of the
Cimmerian blocks. While...
-
Carboniferous to
Early Permian,
Cimmerian terranes opened Meso-Tethys Ocean;
Sibumasu and
Qiangtang were
added to south-east Asia
during Late
Permian and Early...
- 2008.06.004. Ueno, K. (2003). "The
Permian fusulinoidean faunas of the
Sibumasu and
Baoshan blocks:
their implications for the
paleogeographic and paleoclimatologic...
-
continental blocks from Gondwanaland.
These include the
South China, Indochina,
Sibumasu, and West
Burma blocks,
which amalgamated to form the
Southeast Asian continent...
- Gondwanaland. The
continental plate has been
variously termed: Shan-Thai,
Sibumasu, or Sinoburmalaya. This
continental block harbors features of glaciogenic...
-
reactivated due to the
collision between the
Indochina block and the Qiangtang-
Sibumasu terrane in the Tri****ic. The most
important mineral resources in the South...
