Discovery of coesite from Indus Suture Zone (ISZ), Ladakh, India

Evidence for deep subduction

Himanshu K. Sachani, Barun K. Mukherjee, Yoshihide Ogasawara, Shigenori Maruyama, Haruhito Ishida, Atsumi Muko, Nobuhiro Yoshioka

Research output: Contribution to journalArticle

65 Citations (Scopus)

Abstract

Coesite, the high-pressure polymorph of quartz has been identified for the first time in the Tso-Morari Crystalline Complex, Ladakh (India) in the Himalayan belt. The preservation of coesite grains as inclusions in garnet within eclogite boudins indicates the existence of UHP metamorphism in this continental collision setting. The coesite was identified optically and its presence confirmed by its characteristic Raman bands. Both coesite and polycrystalline quartz inclusions exhibit prominent radial fractures in their host garnet. The silica inclusions (monomineralic coesite, monomineralic quartz and bimineralic quartz+coesite) are associated with various textural features and well-developed chemical zonation within the garnet, which show the prograde nature of the UHP metamorphism. Preliminary P-T estimates suggest that the coesite growth took place at pressure > 28 kbar (> 90 km depth) and temperatures > 640°C. Significantly, the coesite inclusions are interpreted as having suffered decompression during exhumation without changing to quartz, most likely due to the rapid uplift. This finding also indicates deep subduction of the Indian plate beneath the Asian continent, The occurrence of coesite and subduction of the Indian plate was essentially governed by a low geothermal gradient which occurred prior to rapid exhumation. This was vital for generating the coherent picture of metamorphism and exposure of UHP rocks.

Original languageEnglish
Pages (from-to)235-240
Number of pages6
JournalEuropean Journal of Mineralogy
Volume16
Issue number2
DOIs
Publication statusPublished - Mar 2004
Externally publishedYes

Fingerprint

coesite
Quartz
suture zone
subduction
Garnets
quartz
garnet
metamorphism
Indian plate
exhumation
Polymorphism
Silicon Dioxide
Rocks
continental collision
geothermal gradient
Crystalline materials
decompression
eclogite
zonation
silica

Keywords

  • Coesite
  • Garnet
  • Raman spectroscopy
  • Tso-Morari
  • UHP eclogite
  • Western Himalaya

ASJC Scopus subject areas

  • Geochemistry and Petrology

Cite this

Sachani, H. K., Mukherjee, B. K., Ogasawara, Y., Maruyama, S., Ishida, H., Muko, A., & Yoshioka, N. (2004). Discovery of coesite from Indus Suture Zone (ISZ), Ladakh, India: Evidence for deep subduction. European Journal of Mineralogy, 16(2), 235-240. https://doi.org/10.1127/0935-1221/2004/0016-0235

Discovery of coesite from Indus Suture Zone (ISZ), Ladakh, India : Evidence for deep subduction. / Sachani, Himanshu K.; Mukherjee, Barun K.; Ogasawara, Yoshihide; Maruyama, Shigenori; Ishida, Haruhito; Muko, Atsumi; Yoshioka, Nobuhiro.

In: European Journal of Mineralogy, Vol. 16, No. 2, 03.2004, p. 235-240.

Research output: Contribution to journalArticle

Sachani, HK, Mukherjee, BK, Ogasawara, Y, Maruyama, S, Ishida, H, Muko, A & Yoshioka, N 2004, 'Discovery of coesite from Indus Suture Zone (ISZ), Ladakh, India: Evidence for deep subduction', European Journal of Mineralogy, vol. 16, no. 2, pp. 235-240. https://doi.org/10.1127/0935-1221/2004/0016-0235
Sachani, Himanshu K. ; Mukherjee, Barun K. ; Ogasawara, Yoshihide ; Maruyama, Shigenori ; Ishida, Haruhito ; Muko, Atsumi ; Yoshioka, Nobuhiro. / Discovery of coesite from Indus Suture Zone (ISZ), Ladakh, India : Evidence for deep subduction. In: European Journal of Mineralogy. 2004 ; Vol. 16, No. 2. pp. 235-240.
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