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Shan-Thai Block

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Journal Article
Published: 01 May 2005
Journal of the Geological Society (2005) 162 (3): 481–484.
... the Jurassic and Early Cretaceous, at a time when that part of the world was isolated from other land masses. The occurrence of a euhelopodid in the Jurassic of the ShanThai Block supports the idea of a collision of the ShanThai Block with the Indochina Block, thus establishing connections with ‘mainland...
FIGURES
Journal Article
Published: 01 January 2005
Journal of the Geological Society (2005) 162 (1): 51–63.
...Brady P. Rhodes; Richard Conejo; Teekayu Benchawan; Susan Titus; Ross Lawson Abstract The Chiang Mai basin is the largest of a zone of rift basins that define the Northern Thailand Basin and Range Province. This province lies within the Shan Thai block of NW Indochina that extruded out of the India...
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Journal Article
Published: 01 November 2002
Geological Magazine (2002) 139 (6): 687–697.
... the Middle and Late Jurassic of China and Central Asia. This supports a Middle Jurassic age for the locality and suggests that the Sibumasu (Shan-Thai) block was in contact with the Asian mainland by that time. § Author for correspondence: Dr H. Tong, e-mail: eric.buffetaut@wanadoo.fr 20 06...
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Journal Article
Published: 01 September 2000
Journal of Paleontology (2000) 74 (5): 789–811.
...KATSUO SASHIDA; HISAYOSHI IGO; SHUKO ADACHI; KATSUMI UENO; YOSHIMICHI KAJIWARA; NIKORN NAKORNSRI; APSORN SARDSUD Abstract Moderately well-preserved Late Permian to Middle Triassic radiolarians are identified in chert beds that occur in the Shan-Thai Block of northern Thailand. These radiolarians...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2004
DOI: 10.1144/GSL.SP.2004.226.01.15
EISBN: 9781862394742
... and the surrounding regions (compiled dataset in Table 2 ). The Late Jurassic–Cretaceous palaeopoles for the Indochina, ShanThai and South China blocks were plotted, along with the synthetic apparent polar wander path for Eurasia ( Besse & Courtillot 1991 ), on a Lambert equal- area projection diagram ( Fig. 5...
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Series: Geological Society, London, Memoirs, Geological Society, London, Memoirs
Published: 01 January 2005
DOI: 10.1144/GSL.MEM.2005.031.01.14
EISBN: 9781862394063
... by the Gigantopteris flora of Jengka Pass ( Kon'no & Asama 1970 ; Hutchison 1994 ), related to those of the North and South China blocks, but with no relationship to the flora and fauna of Gondwana. To this core was added the Shan-Thai or Sibumasu Block, which separated from Gondwana in the Permian...
FIGURES
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2009
DOI: 10.1144/SP315.5
EISBN: 9781862395633
... a hiatus within the Jurassic. There is therefore no clear relationship between the Indosinian Orogeny and the Triassic collision of the Sibumasu (also referred to as Shan-Thai) and Indochina Blocks and the subsequent deposition of the Khorat Group in a Late Triassic–Early Cretaceous thermal sag basin...
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Series: Geological Society, London, Memoirs, Geological Society, London, Memoirs
Published: 01 January 2015
DOI: 10.1144/M45.08
EISBN: 9781862397101
... Belt terrane (see Chapter 2 ). Its western boundary is marked by the dextral Shan Fault (also known as the Mergui Fault in Thailand), and the shelf is located in an overall back-arc setting on continental crust. This shelf area is designated as shallow-water licence blocks M12 and M13 in the north...
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Journal Article
Journal: Economic Geology
Published: 01 June 2003
Economic Geology (2003) 98 (4): 773–785.
... the deposit, and detailed mapping and logging of drill core in this period has generated a much-improved understanding of the setting and controls of the zinc mineralization. The Padaeng deposit is situated in the Shan-Thai or Sibumasu terrane, a crustal block that includes western Thailand and eastern...
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Journal Article
Journal: Geology
Published: 01 October 1987
Geology (1987) 15 (10): 907–910.
... are probably pre-Permian in age. The Nan River belt forms part of the suture between the Indosinian and Shan-Thai cratonic blocks and is inferred to correlate with the Changning-Shuangjiang suture zone in southern China. Geological Society of America 1987 Note: Additional material for this article...
Journal Article
Published: 01 May 2000
Journal of the Geological Society (2000) 157 (3): 553–563.
... rocks of similar age occur in the Loei–Phetchabun area east of the Nan River suture zone ( Fig. 1). In many tectonic models, these two belts have been used to infer the former presence of two contemporaneous subduction zones, one (Lampang) dipping west under the ShanThai block, and the other...
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Journal Article
Published: 01 January 2005
Micropaleontology (2005) 51 (1): 39–57.
... in the area. The radiolarian faunas are systematically described and relationships between them and fauna from adjacent radiolarian provinces are discussed. These cherts with their radiolarian faunas are evidence for the presence of a wide paleo-ocean once existed between Shan-Thai and Indochina continental...
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Journal Article
Published: 06 October 2015
Journal of the Geological Society (2016) 173 (2): 249–264.
... accepted (e.g. Bunopas 1981 ; Metcalfe 1984 , 1986 , 1988 , 1999 , 2002 , 2011 ; Hutchison 1989 ; Sone & Metcalfe 2008 ; Barber et al . 2011 ). However, while accepting that chronology, a different name, the ShanThai block, was introduced by Bunopas (1981) and Bunopas & Vella (1978...
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Image
Index map of northern Thailand. Inset shows the regional tectonic setting o...
Published: 01 January 2005
Fig. 1.  Index map of northern Thailand. Inset shows the regional tectonic setting of the Shan Thai block. Adapted from Barr et al . (2002) .
Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 13 February 2019
Lithosphere (2019) 11 (3): 333–347.
... ), including: (1) the Baoshan, Simao, and Shan Thai (Sibumasu) blocks represent the southeastern continuation of the Qiangtang block; (2) the Simao block represents an extension of the Qiangtang block, whereas the Baoshan and Shan Thai (Sibumasu) blocks correlate with the Lhasa block; (3) the Qiangtang block...
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Image
Palaeogeographical map of the eastern Tethys in the Late Jurassic (simplifi...
Published: 01 May 2005
Fig. 3.  Palaeogeographical map of the eastern Tethys in the Late Jurassic (simplified after Metcalfe 1998 ), showing the distribution of euhelopodid sauropods (•) in Asia. I, Indochina Block; SC, South China Block; ST, ShanThai Block.
Journal Article
Published: 09 September 2020
Geological Magazine (2021) 158 (5): 905–929.
...Hidetoshi Hara; Tetsuya Tokiwa; Toshiyuki Kurihara; Thasinee Charoentitirat; Apsorn Sardsud Abstract Detrital zircon U–Pb ages for sediments in and around the Palaeo-Tethyan convergence zone in northern Thailand provide constraints for tectonic interpretations of the Indochina Block, the Sibumasu...
Journal Article
Journal: GSA Bulletin
Published: 11 May 2017
GSA Bulletin (2017) 129 (9-10): 1100–1122.
.... , and Otofuji , Y. , 2007 , Internal deformation of the Shan-Thai block inferred from paleomagnetism of Jurassic sedimentary rocks in northern Thailand : Journal of Asian Earth Sciences , v. 30 , no. 3–4 , p. 530 – 541 , doi:10.1016/j.jseaes.2007.01.002. Appel , E. , Crouzet , C...
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Series: Geological Society, London, Memoirs, Geological Society, London, Memoirs
Published: 01 January 2015
DOI: 10.1144/M45.06
EISBN: 9781862397101
... are marked on our maps and are labelled as the Shan and Mergui faults, as these appear to be the ‘labels’ most commonly used for these features. We do however believe this is somewhat confusing, since an assumption that the Shan Fault labelled in the offshore on our Figure 6.5 must be connected...
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Image
Top: Contour plot of crustal thickness in China area. Bottom:  Pn  velocity...
Published: 01 April 2004
Figure 5. Top: Contour plot of crustal thickness in China area. Bottom: Pn velocity in China area; 1, Tarim Basin; 2, Ordos Basin; 3, Songliao Basin; 4, Sichuan Basin; 5, Shan Thai Block; 6, Khorat Basin.