Geology of the Kokchetav UHP-HP metamorphic belt, Northern Kazakhstan

Y. Kaneko, S. Maruyama, M. Terabayashi, H. Yamamoto, M. Ishikawa, R. Anma, C. D. Parkinson, T. Ota, Y. Nakajima, I. Katayama, J. Yamamoto, K. Yamauchi

Research output: Contribution to journalArticle

90 Citations (Scopus)

Abstract

Ultrahigh-pressure metamorphic (UHPM) rocks of the Kokchetav Massif of Kazakhstan contain metamorphic microdiamond and coesite inclusions inside rigid capsules such as garnet and zircon. Precambrian protoliths of the UHPM rocks were metamorphosed at around 530 Ma, at pressures of about 7 GPa, which suggests that crustal protoliths were subducted to depths of over 200 km. Primary UHPM minerals are poorly preserved due to partial obliteration by subsequent Barrovian overprint during exhumation and later collision events in Caledonian times. We report the results of detailed mapping of the Kokchetav Massif and use structural data to propose intrusion and exhumation mechanisms for the UHPM rocks. Detailed mapping revealed that many subvertical structures in the ultrahigh-pressure-high-pressure (UHP-HP) units were formed due to later folding. The primary structure appears to be subhorizontal and the total thickness of the UHP rocks is estimated at around 2 km. The first order structure is sandwich-like; that is, the UHP-HP units are separated from underlying low-P metamorphic rocks of the Daulet Series and from feebly metamorphosed to unmetamorphosed sedimentary strata on the top by subhorizontal faults. Kinematic indicators show top-to-the-south sense of shear along the top, and top-to-the-north displacement along the bottom boundaries. These shear senses, together with the observed metamorphic gradients, suggest that the thin UHPM sheet was extruded toward the north. We consider wedge extrusion to have been the most effective mechanism for the exhumation of the UHPM rocks.

Original languageEnglish
Pages (from-to)264-283
Number of pages20
JournalIsland Arc
Volume9
Issue number3
DOIs
Publication statusPublished - 2000
Externally publishedYes

Fingerprint

geology
metamorphic rock
exhumation
protolith
coesite
Caledonian orogeny
extrusion
folding
Precambrian
garnet
zircon
kinematics
collision
mineral
rock

Keywords

  • Exhumation mechanism
  • Kokchetav
  • Ultrahigh pressure metamorphism
  • Wedge extrusion

ASJC Scopus subject areas

  • Earth and Planetary Sciences (miscellaneous)

Cite this

Kaneko, Y., Maruyama, S., Terabayashi, M., Yamamoto, H., Ishikawa, M., Anma, R., ... Yamauchi, K. (2000). Geology of the Kokchetav UHP-HP metamorphic belt, Northern Kazakhstan. Island Arc, 9(3), 264-283. https://doi.org/10.1046/j.1440-1738.2000.00278.x

Geology of the Kokchetav UHP-HP metamorphic belt, Northern Kazakhstan. / Kaneko, Y.; Maruyama, S.; Terabayashi, M.; Yamamoto, H.; Ishikawa, M.; Anma, R.; Parkinson, C. D.; Ota, T.; Nakajima, Y.; Katayama, I.; Yamamoto, J.; Yamauchi, K.

In: Island Arc, Vol. 9, No. 3, 2000, p. 264-283.

Research output: Contribution to journalArticle

Kaneko, Y, Maruyama, S, Terabayashi, M, Yamamoto, H, Ishikawa, M, Anma, R, Parkinson, CD, Ota, T, Nakajima, Y, Katayama, I, Yamamoto, J & Yamauchi, K 2000, 'Geology of the Kokchetav UHP-HP metamorphic belt, Northern Kazakhstan', Island Arc, vol. 9, no. 3, pp. 264-283. https://doi.org/10.1046/j.1440-1738.2000.00278.x
Kaneko Y, Maruyama S, Terabayashi M, Yamamoto H, Ishikawa M, Anma R et al. Geology of the Kokchetav UHP-HP metamorphic belt, Northern Kazakhstan. Island Arc. 2000;9(3):264-283. https://doi.org/10.1046/j.1440-1738.2000.00278.x
Kaneko, Y. ; Maruyama, S. ; Terabayashi, M. ; Yamamoto, H. ; Ishikawa, M. ; Anma, R. ; Parkinson, C. D. ; Ota, T. ; Nakajima, Y. ; Katayama, I. ; Yamamoto, J. ; Yamauchi, K. / Geology of the Kokchetav UHP-HP metamorphic belt, Northern Kazakhstan. In: Island Arc. 2000 ; Vol. 9, No. 3. pp. 264-283.
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AU - Ishikawa, M.

AU - Anma, R.

AU - Parkinson, C. D.

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AB - Ultrahigh-pressure metamorphic (UHPM) rocks of the Kokchetav Massif of Kazakhstan contain metamorphic microdiamond and coesite inclusions inside rigid capsules such as garnet and zircon. Precambrian protoliths of the UHPM rocks were metamorphosed at around 530 Ma, at pressures of about 7 GPa, which suggests that crustal protoliths were subducted to depths of over 200 km. Primary UHPM minerals are poorly preserved due to partial obliteration by subsequent Barrovian overprint during exhumation and later collision events in Caledonian times. We report the results of detailed mapping of the Kokchetav Massif and use structural data to propose intrusion and exhumation mechanisms for the UHPM rocks. Detailed mapping revealed that many subvertical structures in the ultrahigh-pressure-high-pressure (UHP-HP) units were formed due to later folding. The primary structure appears to be subhorizontal and the total thickness of the UHP rocks is estimated at around 2 km. The first order structure is sandwich-like; that is, the UHP-HP units are separated from underlying low-P metamorphic rocks of the Daulet Series and from feebly metamorphosed to unmetamorphosed sedimentary strata on the top by subhorizontal faults. Kinematic indicators show top-to-the-south sense of shear along the top, and top-to-the-north displacement along the bottom boundaries. These shear senses, together with the observed metamorphic gradients, suggest that the thin UHPM sheet was extruded toward the north. We consider wedge extrusion to have been the most effective mechanism for the exhumation of the UHPM rocks.

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