Singtuen Vimoltip, Phajan Sirinthorn, Anumart Apussorn, Phajuy Burapha, Srijanta Kantapong, Promkotra Sarunya
Department of Geotechnology, Faculty of Technology, Khon Kaen University, 123 Mitrparp Rd., Nai Muang, Muang Khon Kaen, Khon Kaen 40002 Thailand.
Department of Geological Sciences, Faculty of Science, Chiang Mai University, 239 Huai Kaew Rd., Suthep, Muang Chiang Mai, Chiang Mai 50200 Thailand.
Heliyon. 2021 Dec 20;7(12):e08619. doi: 10.1016/j.heliyon.2021.e08619. eCollection 2021 Dec.
Lava Durian Sisaket is the first geographically identified (GI) fruit related to the volcano in Thailand and distributed in three districts of Sisaket Province, the southernmost edge of the Khorat Plateau. The parent rocks of orchards are important for the description of soil and rock relation with respect to mineralogical and geochemical characteristics. This work aims to study lithology, mineralogy, and geochemistry of basaltic rocks, parent rocks of in situ soil in these orchards, and delineate the existing basaltic soil models. The several orchards are covered by reddish-brown to brown in situ soils, weathered from mafic volcanic rocks: porphyritic olivine basalt, vesicular olivine basalt, and nephelinite. The microscopic image analysis, XRD, and MiniSEM-EDS are used to classify mineralogy, while XRF and analysis of large and rare elements in ICP-MS/ICP-OES were used to determine parental rocks geochemistry and alteration. The olivine basalts comprise forsterite microphenocrysts associated with bytownite, diopside, augite, pigeonite, and ilmenite groundmass, while nephelinite is composed of nepheline groundmass and bytownite-labradorite, diopside, augite, pigeonite, and ilmenite crystals. In addition, these basalts display high alteration rates, especially olivine highly altered to iddingsite. According to the geochemical data, Sisaket's basalts were identified as alkali basalt and nepheline basanite with high LILEs and LREEs (La, Nd, Pr, Gd, Eu). The kaolinite, smectite, and illite are altered from felsic minerals, while the chlorite and iddingsite are from mafic minerals. The mineralogical analyses classified secondary phyllosilicates related to low-moderate temperature hydrothermal fluid, very high cation exchange capacity (H, K, Ca, Mg), and tropical weathering. The alkaline and high alkaline basalts, presenting as parent rocks, are one of the parameters that produced good nitisal soil of Sisaket's agricultural areas.
洛瓦榴莲色吉是泰国第一种与火山相关的地理标志(GI)水果,分布在呵叻高原最南端色吉府的三个区。果园的母岩对于描述土壤与岩石在矿物学和地球化学特征方面的关系很重要。这项工作旨在研究这些果园原地土壤的母岩玄武岩的岩性、矿物学和地球化学,并勾勒出现有的玄武岩土壤模型。几个果园覆盖着红棕色至棕色的原地土壤,这些土壤由镁铁质火山岩风化而成:斑状橄榄玄武岩、气孔状橄榄玄武岩和霞石岩。利用显微镜图像分析、XRD和MiniSEM-EDS对矿物学进行分类,而XRF以及ICP-MS/ICP-OES中大量和稀有元素的分析则用于确定母岩的地球化学和蚀变情况。橄榄玄武岩由与倍长石、透辉石、普通辉石、易变辉石和钛铁矿基质相关的镁橄榄石微晶组成,而霞石岩由霞石基质和倍长石-拉长石、透辉石、普通辉石、易变辉石和钛铁矿晶体组成。此外,这些玄武岩显示出高蚀变率,尤其是橄榄石高度蚀变为伊丁石。根据地球化学数据,色吉的玄武岩被确定为碱性玄武岩和霞石碧玄岩,具有高的大离子亲石元素(LILEs)和轻稀土元素(LREEs,如La、Nd、Pr、Gd、Eu)。高岭石、蒙脱石和伊利石由长英质矿物蚀变而来,而绿泥石和伊丁石则来自镁铁质矿物。矿物学分析将与中低温热液流体、非常高的阳离子交换容量(H、K、Ca、Mg)和热带风化有关的次生层状硅酸盐进行了分类。作为母岩的碱性和高碱性玄武岩是色吉农业区形成优质泥质土壤的参数之一。