JpGU-AGU Joint Meeting 2017

講演情報

[JJ] ポスター発表

セッション記号 S (固体地球科学) » S-RD 資源・鉱床・資源探査

[S-RD39] [JJ] 資源地質学

2017年5月25日(木) 13:45 〜 15:15 ポスター会場 (国際展示場 7ホール)

コンビーナ:大竹 翼(北海道大学大学院工学研究院 環境循環システム部門)、野崎 達生(海洋研究開発機構海底資源研究開発センター)、実松 健造(国立研究開発法人 産業技術総合研究所 地圏資源環境研究部門 鉱物資源研究グループ)、高橋 亮平(秋田大学大学院国際資源学研究科)

[SRD39-P07] Petrochemistry of Plutonic Rocks along Loei Fold Belt, Northeastern Thailand

*Patchawee Nualkhao1Ryohei Takahashi1Akira Imai1Punya Charusiri2 (1.Akita University、2.Chulalongkorn University)

キーワード:Loei Fold Belt, Geochemistry, Petrology, Calc-alkaline, Thailand

Petrography and geochemistry of Permo-Triassic plutonic rocks from different provinces along the Loei Fold Belt, northeastern Thailand were studied. The Loei Fold Belt is an 800-km north-south trending fold belt that hosts an epithermal Au and several skarn Cu-Au deposits. Petrographic analysis of the granodiorites, diorites and granites in the area shows that the rocks consist mainly of quartz, plagioclase, hornblende and biotite. Orthoclase feldspars has been noted from samples in the Loei Province. Accessory minerals such as magnetite and ilmenite were also present. Magnetic susceptibilities of granitoids vary from 0.01 to 11.14×10-3 SI in the Loei Province, from 0.07 to 9.9×10-3 SI in the Petchabun Province and 0.02 to 2.81×10-3 in the Chantaburi Province. Concentrations of major elements suggest that these intermediate to acid igneous rocks have calc-alkaline affinities. Trace element geochemistry upon normalization to chondrite shows moderately elevated LREEs and relatively flat HREEs, with distinct depletion of Eu. Plotting concentrations of Rb versus Y/Nb and Nb/Y in tectonic discrimination diagrams for granitoids show that the rocks formed in volcanic-arc setting. New age data from radiometric K-Ar dating of orthoclase from granodiorite in the provinces of Loei and Nakhon Sawan yielded ages of 171 and 221 Ma, respectively. Age data of hornblende separated from diorite in Lopburi Province yielded ages of 219 Ma. Sulfur isotope data of pyrite separated from limestone and skarn deposit in Wang Saphung, Loei Province, show negative values of δ34S (CDT) from -9 to +1‰. The sulfur isotope values suggest that the magma had been influenced by light biogenic sulfur from local country rocks.