The Shan–Thai or Sibumasu Terrane is a mass of continental crust extending from Tibet into Southeast Asia sharing a similar geological history. The Shan–Thai Terrane rifted from Australia in the Permian and collided with the Indochina terrane in the Triassic. It extends from Malaysia, through peninsular Thailand, Myanmar, West Yunnan, to Lhasa.
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| - Shan-Thai Terrane (it)
- Shan–Thai Terrane (en)
- 掸泰地体 (zh)
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| - Lo Shan–Thai Terrane o Sibumasu Terrane, è una porzione di crosta continentale che si estende dal Tibet all'Asia sudorientale condividendo una storia geologica simile. Lo Shan–Thai Terrane si è separato dall'Australia durante il Permiano e andò a collidere con il terrane dell'Indocina (o microcontinente Cimmeria) nel corso del Triassico. (it)
- 掸泰地块，又称掸邦地块、滇缅马苏地块（Sibumasu massif）、滇缅马来亚地块（Sinoburmalaya massif），中国境内称为保山地块。位于缅甸东部掸邦的一个近南北向的长条形地体。北起中国云南保山，向南经过缅甸、泰国、马来半岛，南至苏门答腊岛，长4000km。 (zh)
- The Shan–Thai or Sibumasu Terrane is a mass of continental crust extending from Tibet into Southeast Asia sharing a similar geological history. The Shan–Thai Terrane rifted from Australia in the Permian and collided with the Indochina terrane in the Triassic. It extends from Malaysia, through peninsular Thailand, Myanmar, West Yunnan, to Lhasa. (en)
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| - The Shan–Thai or Sibumasu Terrane is a mass of continental crust extending from Tibet into Southeast Asia sharing a similar geological history. The Shan–Thai Terrane rifted from Australia in the Permian and collided with the Indochina terrane in the Triassic. It extends from Malaysia, through peninsular Thailand, Myanmar, West Yunnan, to Lhasa. Shan–Thai is c. 4,000 km (2,500 mi) long and bounded by the Indochina terrane to the east and the South China terrane to the north. It is one of a series of continental blocks or terranes that were rifted off eastern Gondwana during the Ordovician (495 to 443 Ma), long before the formation of Pangaea. Today these blocks form south-east Asia but the different timing of their journeys has given them distinct geologic histories. Shan–Thai was an archipelago on the Paleo-Tethys Ocean spread over several latitudes. It can therefore be subdivided into several portions with different palaeo-geographical histories. The internal "Thai" elements, bordering the Indochina block, are of Cathaysian type and characterised by palaeo-tropical warm-water facies. The external "Shan" part has Gondwanan cold-water facies whilst the central "Sibumasu" part is transitional between the other two.The internal parts of Shan–Thai merged with Laurasia 265 Ma when the Nan-Uttaradit suture closed.Oceanic basins separated the other elements of Shan–Thai until the Late Triassic–Early Jurassic Late Indochina Orogeny. The collision between India and Eurasia during the Oligocene and Miocene resulted in clockwise rotation of south-west Asia, severe deformation of south-east Asia, and the extrusion of Shan–Thai and Indochina blocks. These two blocks are still crisscrossed by the faults from this collision. (en)
- Lo Shan–Thai Terrane o Sibumasu Terrane, è una porzione di crosta continentale che si estende dal Tibet all'Asia sudorientale condividendo una storia geologica simile. Lo Shan–Thai Terrane si è separato dall'Australia durante il Permiano e andò a collidere con il terrane dell'Indocina (o microcontinente Cimmeria) nel corso del Triassico. (it)
- 掸泰地块，又称掸邦地块、滇缅马苏地块（Sibumasu massif）、滇缅马来亚地块（Sinoburmalaya massif），中国境内称为保山地块。位于缅甸东部掸邦的一个近南北向的长条形地体。北起中国云南保山，向南经过缅甸、泰国、马来半岛，南至苏门答腊岛，长4000km。 (zh)
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