Singtuen Vimoltip, Phajan Sirinthorn
Department of Geotechnology, Faculty of Technology, Khon Kaen University, 123 Moo 16 Mittraphap Rd., Nai-Muang, Muang, Khon Kaen, Thailand.
Data Brief. 2021 Nov 3;39:107540. doi: 10.1016/j.dib.2021.107540. eCollection 2021 Dec.
This data article presents mineralogical and geochemical data of high alkaline basalts in Sisaket province, the southern part of Khorat Plateau, NE Thailand. Under the polarized light microscope, the photomicrographs divided the basalts into olivine basalt and alkaline basalt with four textures: aphanitic, porphyritic, vesicular, and diabase. These basaltic rocks comprise olivine microphenocrysts associated with labradorite-anorthite (An), clinopyroxene, opaque minerals groundmass. In addition, nepheline is only found in alkaline basalt as groundmass. Major oxides (NaO+KO and SiO) suggest that Sisaket basalts are basalt, basanite, trachy basalt, and basaltic trachy-andesite. High ratio Nb/Y and low Zr/Ti classify these basalts as alkaline basalt and basanite.
本文献展示了泰国东北部呵叻高原南部四色菊府高碱性玄武岩的矿物学和地球化学数据。在偏光显微镜下,显微照片将玄武岩分为橄榄玄武岩和碱性玄武岩,具有四种结构:隐晶质、斑状、气孔状和辉绿岩结构。这些玄武岩岩石包含与拉长石 - 钙长石(An)、单斜辉石、不透明矿物基质相关的橄榄石微晶。此外,霞石仅在碱性玄武岩中作为基质被发现。主要氧化物(NaO + KO 和 SiO)表明,四色菊玄武岩为玄武岩、碧玄岩、粗面玄武岩和玄武质粗面安山岩。高 Nb/Y 比和低 Zr/Ti 将这些玄武岩归类为碱性玄武岩和碧玄岩。