Geochronological, elemental and Sr-Nd-Hf-O isotopic constraints on the petrogenesis of the Triassic post-collisional granitic rocks in NW Thailand and its Paleotethyan implications

Yuejun Wang, Huiying He, Peter A. Cawood, Boontarika Srithai, Qinglai Feng, Weiming Fan, Yuzhi Zhang, Xin Qian

Research output: Contribution to journalArticleResearchpeer-review

Abstract

New U-Pb geochronological, petrologic, elemental and Sr-Nd-Hf-O isotopic data for the granites from the Inthanon and Sukhothai zones in NW Thailand in conjunction with correlations with SW China are presented to constrain the age and position of the Paleotethys Ocean in this region and the associated assembly of Southeast Asia. The geochronological data show that the granitic rocks in the Inthanon and Sukhothai zones, herein named Group 1 and Group 2 granites, respectively, yield similar crystallization ages of 230-200 Ma. Group 1 samples are characterized by monzogranite and granite with I- and S-type geochemical affinity and Group 2 samples by I-type monzogranite and granodiorite. They have generally similar chondrite-normalized REE and PM-normalized multi-element patterns but distinct Sr-Nd-Hf-O isotopic compositions. Group 1 samples have slightly higher initial 87Sr/86Sr ratios (0.7111-0.7293) but lower εNd(t) values (− 11.1 to − 14.1) than those of Group 2 samples (87Sr/86Sr(i) = 0.7073-0.7278 and εNd(t) = − 8.3 to − 11.0). Group 1 samples show the lower εHf(t) values (− 5.4 to − 18.2), older TDM (1.62-2.40 Ga) and higher δ18O values (+ 7.95 to + 9.94) than those of Group 2 samples (εHf(t) of − 11.1 to + 4.80, TDM of 0.96-1.95 Ga and δ18O of + 4.95 to + 7.98) for the Triassic crystallization zircons. These geochemical signatures are similar to the Kwangsian and Indosinian granites in the South China and Indochina blocks but distinct from those of the Gangdese I-type granite and Sibumasu Paleozoic granite. Our data suggest that Group 1 samples mainly originated from the early Paleozoic supracrustal rocks containing metapelite and metavolcanic components, which had previously experienced the surface weathering. Group 2 samples were derived from a hybridized source of an old metamorphic and a newly underplated mafic component. Synthesis of our data with available regional observations indicates that the Inthanon zone represents the main suture zone of the eastern Paleotethyan Ocean in NW Thailand and links with the Changning-Menglian suture zone in SW Yunnan (SW China). In NW Thailand, a switch from the eastward subduction of the Paleotethyan oceanic plate to the collision of the Sibumasu with Indochina blocks occurred at ~ 237 Ma, and syn- and post-collisional time being at ~ 237-230 Ma and ~ 200-230 Ma, respectively. The late Triassic granites in the Inthanon and Sukhothai zones are representative of the post-collisional magmatic products.

Original languageEnglish
Pages (from-to)264-286
Number of pages23
JournalLithos
Volume266-267
DOIs
Publication statusPublished - 1 Dec 2016
Externally publishedYes

Keywords

  • Eastern Paleotethyan evolution
  • Elemental and Sr-Nd-Hf-O isotopic data
  • Late Triassic granite
  • NW Thailand
  • Post-collisional collapse
  • Zircon U-Pb dating

Cite this

Wang, Yuejun ; He, Huiying ; Cawood, Peter A. ; Srithai, Boontarika ; Feng, Qinglai ; Fan, Weiming ; Zhang, Yuzhi ; Qian, Xin. / Geochronological, elemental and Sr-Nd-Hf-O isotopic constraints on the petrogenesis of the Triassic post-collisional granitic rocks in NW Thailand and its Paleotethyan implications. In: Lithos. 2016 ; Vol. 266-267. pp. 264-286.
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abstract = "New U-Pb geochronological, petrologic, elemental and Sr-Nd-Hf-O isotopic data for the granites from the Inthanon and Sukhothai zones in NW Thailand in conjunction with correlations with SW China are presented to constrain the age and position of the Paleotethys Ocean in this region and the associated assembly of Southeast Asia. The geochronological data show that the granitic rocks in the Inthanon and Sukhothai zones, herein named Group 1 and Group 2 granites, respectively, yield similar crystallization ages of 230-200 Ma. Group 1 samples are characterized by monzogranite and granite with I- and S-type geochemical affinity and Group 2 samples by I-type monzogranite and granodiorite. They have generally similar chondrite-normalized REE and PM-normalized multi-element patterns but distinct Sr-Nd-Hf-O isotopic compositions. Group 1 samples have slightly higher initial 87Sr/86Sr ratios (0.7111-0.7293) but lower εNd(t) values (− 11.1 to − 14.1) than those of Group 2 samples (87Sr/86Sr(i) = 0.7073-0.7278 and εNd(t) = − 8.3 to − 11.0). Group 1 samples show the lower εHf(t) values (− 5.4 to − 18.2), older TDM (1.62-2.40 Ga) and higher δ18O values (+ 7.95 to + 9.94) than those of Group 2 samples (εHf(t) of − 11.1 to + 4.80, TDM of 0.96-1.95 Ga and δ18O of + 4.95 to + 7.98) for the Triassic crystallization zircons. These geochemical signatures are similar to the Kwangsian and Indosinian granites in the South China and Indochina blocks but distinct from those of the Gangdese I-type granite and Sibumasu Paleozoic granite. Our data suggest that Group 1 samples mainly originated from the early Paleozoic supracrustal rocks containing metapelite and metavolcanic components, which had previously experienced the surface weathering. Group 2 samples were derived from a hybridized source of an old metamorphic and a newly underplated mafic component. Synthesis of our data with available regional observations indicates that the Inthanon zone represents the main suture zone of the eastern Paleotethyan Ocean in NW Thailand and links with the Changning-Menglian suture zone in SW Yunnan (SW China). In NW Thailand, a switch from the eastward subduction of the Paleotethyan oceanic plate to the collision of the Sibumasu with Indochina blocks occurred at ~ 237 Ma, and syn- and post-collisional time being at ~ 237-230 Ma and ~ 200-230 Ma, respectively. The late Triassic granites in the Inthanon and Sukhothai zones are representative of the post-collisional magmatic products.",
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Geochronological, elemental and Sr-Nd-Hf-O isotopic constraints on the petrogenesis of the Triassic post-collisional granitic rocks in NW Thailand and its Paleotethyan implications. / Wang, Yuejun; He, Huiying; Cawood, Peter A.; Srithai, Boontarika; Feng, Qinglai; Fan, Weiming; Zhang, Yuzhi; Qian, Xin.

In: Lithos, Vol. 266-267, 01.12.2016, p. 264-286.

Research output: Contribution to journalArticleResearchpeer-review

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T1 - Geochronological, elemental and Sr-Nd-Hf-O isotopic constraints on the petrogenesis of the Triassic post-collisional granitic rocks in NW Thailand and its Paleotethyan implications

AU - Wang, Yuejun

AU - He, Huiying

AU - Cawood, Peter A.

AU - Srithai, Boontarika

AU - Feng, Qinglai

AU - Fan, Weiming

AU - Zhang, Yuzhi

AU - Qian, Xin

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N2 - New U-Pb geochronological, petrologic, elemental and Sr-Nd-Hf-O isotopic data for the granites from the Inthanon and Sukhothai zones in NW Thailand in conjunction with correlations with SW China are presented to constrain the age and position of the Paleotethys Ocean in this region and the associated assembly of Southeast Asia. The geochronological data show that the granitic rocks in the Inthanon and Sukhothai zones, herein named Group 1 and Group 2 granites, respectively, yield similar crystallization ages of 230-200 Ma. Group 1 samples are characterized by monzogranite and granite with I- and S-type geochemical affinity and Group 2 samples by I-type monzogranite and granodiorite. They have generally similar chondrite-normalized REE and PM-normalized multi-element patterns but distinct Sr-Nd-Hf-O isotopic compositions. Group 1 samples have slightly higher initial 87Sr/86Sr ratios (0.7111-0.7293) but lower εNd(t) values (− 11.1 to − 14.1) than those of Group 2 samples (87Sr/86Sr(i) = 0.7073-0.7278 and εNd(t) = − 8.3 to − 11.0). Group 1 samples show the lower εHf(t) values (− 5.4 to − 18.2), older TDM (1.62-2.40 Ga) and higher δ18O values (+ 7.95 to + 9.94) than those of Group 2 samples (εHf(t) of − 11.1 to + 4.80, TDM of 0.96-1.95 Ga and δ18O of + 4.95 to + 7.98) for the Triassic crystallization zircons. These geochemical signatures are similar to the Kwangsian and Indosinian granites in the South China and Indochina blocks but distinct from those of the Gangdese I-type granite and Sibumasu Paleozoic granite. Our data suggest that Group 1 samples mainly originated from the early Paleozoic supracrustal rocks containing metapelite and metavolcanic components, which had previously experienced the surface weathering. Group 2 samples were derived from a hybridized source of an old metamorphic and a newly underplated mafic component. Synthesis of our data with available regional observations indicates that the Inthanon zone represents the main suture zone of the eastern Paleotethyan Ocean in NW Thailand and links with the Changning-Menglian suture zone in SW Yunnan (SW China). In NW Thailand, a switch from the eastward subduction of the Paleotethyan oceanic plate to the collision of the Sibumasu with Indochina blocks occurred at ~ 237 Ma, and syn- and post-collisional time being at ~ 237-230 Ma and ~ 200-230 Ma, respectively. The late Triassic granites in the Inthanon and Sukhothai zones are representative of the post-collisional magmatic products.

AB - New U-Pb geochronological, petrologic, elemental and Sr-Nd-Hf-O isotopic data for the granites from the Inthanon and Sukhothai zones in NW Thailand in conjunction with correlations with SW China are presented to constrain the age and position of the Paleotethys Ocean in this region and the associated assembly of Southeast Asia. The geochronological data show that the granitic rocks in the Inthanon and Sukhothai zones, herein named Group 1 and Group 2 granites, respectively, yield similar crystallization ages of 230-200 Ma. Group 1 samples are characterized by monzogranite and granite with I- and S-type geochemical affinity and Group 2 samples by I-type monzogranite and granodiorite. They have generally similar chondrite-normalized REE and PM-normalized multi-element patterns but distinct Sr-Nd-Hf-O isotopic compositions. Group 1 samples have slightly higher initial 87Sr/86Sr ratios (0.7111-0.7293) but lower εNd(t) values (− 11.1 to − 14.1) than those of Group 2 samples (87Sr/86Sr(i) = 0.7073-0.7278 and εNd(t) = − 8.3 to − 11.0). Group 1 samples show the lower εHf(t) values (− 5.4 to − 18.2), older TDM (1.62-2.40 Ga) and higher δ18O values (+ 7.95 to + 9.94) than those of Group 2 samples (εHf(t) of − 11.1 to + 4.80, TDM of 0.96-1.95 Ga and δ18O of + 4.95 to + 7.98) for the Triassic crystallization zircons. These geochemical signatures are similar to the Kwangsian and Indosinian granites in the South China and Indochina blocks but distinct from those of the Gangdese I-type granite and Sibumasu Paleozoic granite. Our data suggest that Group 1 samples mainly originated from the early Paleozoic supracrustal rocks containing metapelite and metavolcanic components, which had previously experienced the surface weathering. Group 2 samples were derived from a hybridized source of an old metamorphic and a newly underplated mafic component. Synthesis of our data with available regional observations indicates that the Inthanon zone represents the main suture zone of the eastern Paleotethyan Ocean in NW Thailand and links with the Changning-Menglian suture zone in SW Yunnan (SW China). In NW Thailand, a switch from the eastward subduction of the Paleotethyan oceanic plate to the collision of the Sibumasu with Indochina blocks occurred at ~ 237 Ma, and syn- and post-collisional time being at ~ 237-230 Ma and ~ 200-230 Ma, respectively. The late Triassic granites in the Inthanon and Sukhothai zones are representative of the post-collisional magmatic products.

KW - Eastern Paleotethyan evolution

KW - Elemental and Sr-Nd-Hf-O isotopic data

KW - Late Triassic granite

KW - NW Thailand

KW - Post-collisional collapse

KW - Zircon U-Pb dating

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