Geochronological constraints on multiple deformations of the Honam Shear Zone, South Korea and its tectonic implication

Sung Won Kim, Sanghoon Kwon, In Chang Ryu

Research output: Contribution to journalArticle

29 Citations (Scopus)

Abstract

The NE-trending Honam Shear Zone, South Korea, is a tectonic-scale shear zone, consisting of several parallel mylonite zones: Jeonju, Sunchang and Yecheon shear zones. Here we report the sensitive high-resolution ion microprobe (SHRIMP) U-Pb zircon ages from the mylonitic Precambrian orthogneiss and hornblende-biotite granitoid near the Myeongho area within the Yecheon Shear Zone, a representative segment of the Honam Shear Zone. The core and overgrowth parts of the zircons from the foliated hornblende-biotite granitoid yielded ca. 187 Ma and ca. 178 Ma, respectively. The former is interpreted as a timing of emplacement, whereas the latter as a timing of subsequent mylonitization, which is similar to zircon overgrowth age of ca. 179 Ma obtained from mylonitized quartz-feldspar orthogneiss. Muscovite and biotite K-Ar ages of mylonitized Precambrian rocks and foliated granitoids range from 162-168 Ma, 148-155 Ma, and 136 Ma. Our geochronological results, combined with those of previous geochronological and structural studies, suggest that the Honam Shear Zone is a tectonic element created during Middle Jurassic Daebo (or early Yanshanian) Orogeny and lasted possibly as late as at Early Cretaceous in relation to the subduction of the Izanagi Plate under the Asian continent.

Original languageEnglish
Pages (from-to)82-89
Number of pages8
JournalGondwana Research
Volume16
Issue number1
DOIs
Publication statusPublished - 2009 Aug 1

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shear zone
tectonics
biotite
orthogneiss
zircon
granitoid
hornblende
Precambrian
mylonitization
mylonite
ion microprobe
muscovite
orogeny
feldspar
emplacement
subduction
Jurassic
quartz
Cretaceous
rock

All Science Journal Classification (ASJC) codes

  • Geology

Cite this

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abstract = "The NE-trending Honam Shear Zone, South Korea, is a tectonic-scale shear zone, consisting of several parallel mylonite zones: Jeonju, Sunchang and Yecheon shear zones. Here we report the sensitive high-resolution ion microprobe (SHRIMP) U-Pb zircon ages from the mylonitic Precambrian orthogneiss and hornblende-biotite granitoid near the Myeongho area within the Yecheon Shear Zone, a representative segment of the Honam Shear Zone. The core and overgrowth parts of the zircons from the foliated hornblende-biotite granitoid yielded ca. 187 Ma and ca. 178 Ma, respectively. The former is interpreted as a timing of emplacement, whereas the latter as a timing of subsequent mylonitization, which is similar to zircon overgrowth age of ca. 179 Ma obtained from mylonitized quartz-feldspar orthogneiss. Muscovite and biotite K-Ar ages of mylonitized Precambrian rocks and foliated granitoids range from 162-168 Ma, 148-155 Ma, and 136 Ma. Our geochronological results, combined with those of previous geochronological and structural studies, suggest that the Honam Shear Zone is a tectonic element created during Middle Jurassic Daebo (or early Yanshanian) Orogeny and lasted possibly as late as at Early Cretaceous in relation to the subduction of the Izanagi Plate under the Asian continent.",
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Geochronological constraints on multiple deformations of the Honam Shear Zone, South Korea and its tectonic implication. / Kim, Sung Won; Kwon, Sanghoon; Ryu, In Chang.

In: Gondwana Research, Vol. 16, No. 1, 01.08.2009, p. 82-89.

Research output: Contribution to journalArticle

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