Alteration of high alkaline and alkaline basaltic rocks: parent rocks in the Lava Durian orchard, Sisaket Province, NE Thailand

Heliyon

Sirinthorn Phajan¹  Kantapong Srijanta²  Vimoltip Singtuen³  Apussorn Anumart³  Burapha Phajuy³  Sarunya Promkotra³ 

[1] Corresponding author.;Department of Geological Sciences, Faculty of Science, Chiang Mai University, 239 Huai Kaew Rd., Suthep, Muang Chiang Mai, Chiang Mai 50200 Thailand;Department of Geotechnology, Faculty of Technology, Khon Kaen University, 123 Mitrparp Rd., Nai Muang, Muang Khon Kaen, Khon Kaen 40002 Thailand;

关键词: Basalt;    Nephelinite;    Olivine basalt;    Iddingsite;    Hydrothermal;    Geochemistry;   

DOI  :  

来源: DOAJ

【 摘 要 】

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+, Ca2+, Mg2+), 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.

【 授权许可】

Unknown