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Minerals 2021, 11, 1330 9 of 23 Minerals 2021, 11, 1330 9 of 24 Figure 4. Field outcrops and microscopic photographs of basalt in Jiangling depression. (A) Red stomata almond-shaped Figure 4. Field outcrops and microscopic photographs of basalt in Jiangling depression. (A) Red stomata almond- basalt; (B) dense massive basalt; (C) columnar jointed basalt; (D) calcite and quartz veins developed in basalt; (E) inter- shaped basalt; (B) dense massive basalt; (C) columnar jointed basalt; (D) calcite and quartz veins developed in basalt; granular basalt. Olivine undergoes intense alteration, chloritization, and iddingsitization; perpendicular polarized light. (E) intergranular basalt. Olivine undergoes intense alteration, chloritization, and iddingsitization; perpendicular polarized Plagioclase is colorless and transparent and has two groups of complete cleavage; long strip, polarization microscope light. Plagioclase is colorless and transparent and has two groups of complete cleavage; long strip, polarization microscope common twin, interference color level gray, negative low protrusion. (F) Basalt is mainly composed of plagioclase (Pl) common twin, interference color level gray, negative low protrusion. (F) Basalt is mainly composed of plagioclase (Pl) and pyroxene (Px), with weak alteration pairs; perpendicular polarized light. Pyroxene is the most common mineral in and pyroxene (Px), with weak alteration pairs; perpendicular polarized light. Pyroxene is the most common mineral in ultrabasic rocks and mafic rocks. It is greenish black and has two groups of nearly vertical cleavage, often forming irreg- ulatrasbtaespipc erodcfkrsacatnudrems.afic rocks. It is greenish black and has two groups of nearly vertical cleavage, often forming irregular stepped fractures. According to the major element analysis of basalt samples in the Jiangling depres- 4.2.2. Granite sion (Table 2), the SiO2 content in the basalt ranges from 52.86% to 53.10%, with an av- The analysis results of the major element composition of granite around the Jiangling erage value of 52.99%. The Na2O content varies from 3.24% to 3.87%, with an average of depression(Table3)revealthattheSiO contentingraniteishigh,rangingfrom70.33%to 3.48%. The K2O content varies from 1.023% to 1.20%, with an average of 1.09%. The Al2O3 73.05%, with an average of 71.37%; the content of K O varies from 4.64% to 5.35%, with content ranges from 13.03% to 14.00%, with an av2erage of 13.54%. The CaO content an average of 5.04%; the content of Na O varies from 2.88% to 3.62%, with an average of 2 ranges from 6.23% to 8.55%, with an average of 7.34%. 3.20%; the content of Al2O3 varies from 14.10% to 15.14%, with an average of 14.68%; and the content of CaO ranges from 1.26% to 2.04%, with an average of 1.76%.PDF Image | Origin of Lithium Potassium Rich Brines in the Jianghan
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