2015
DOI: 10.1016/j.chemer.2015.04.002
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Chemical and isotopic characteristics and origin of spring waters in the Lanping–Simao Basin, Yunnan, Southwestern China

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Cited by 41 publications
(18 citation statements)
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“…Tachyhydrites and saddle dolomites documented within the Khorat Plateau by El Tabakh(1999;2003), both of which form at high temperatures (>35℃; Huang Keke et al, 2016;Yang et al, 2016), provide evidence for a thermal event during the Cretaceous. Bo (Bo Ying et al, 2015;Bo et al, 2015a) suggested that the Yanjing-Lanping-Simao-northern Laos share geochemical affinities, and the geothermal activity occurred from the north to the south. There are also granite intrusions of an upper Cretaceous extent in the Khorat Plateau (El Tabakh et al, 1999) may indicate the influence of mantle.…”
Section: The Influence Of Non-marine Resourcesmentioning
confidence: 99%
“…Tachyhydrites and saddle dolomites documented within the Khorat Plateau by El Tabakh(1999;2003), both of which form at high temperatures (>35℃; Huang Keke et al, 2016;Yang et al, 2016), provide evidence for a thermal event during the Cretaceous. Bo (Bo Ying et al, 2015;Bo et al, 2015a) suggested that the Yanjing-Lanping-Simao-northern Laos share geochemical affinities, and the geothermal activity occurred from the north to the south. There are also granite intrusions of an upper Cretaceous extent in the Khorat Plateau (El Tabakh et al, 1999) may indicate the influence of mantle.…”
Section: The Influence Of Non-marine Resourcesmentioning
confidence: 99%
“…Although these examples show similar data to the CD-LP-SM springs, the B origin in springs of the study area is different, reflecting a unique geological background and wall-rock type. In addition, the wide distribution of crustal -derived He indicates that water circulation in the Lanping -Simao Basin and northern Laos may be limited above the upper mantle (Bo et al, 2015). Thus, B in springs from the study area is unlikely to have a deep mantle source; instead, a primarily crustal source (volcanic rocks and marine carbonates) is more likely.…”
Section: Comparison With Springs Worldwidementioning
confidence: 92%
“…With regards to weak water-rock interactions, the δ 11 B values of springs in the study area are mainly controlled by the leaching of reservoir host rocks (marine carbonates and volcanic rocks). According to Bo et al (2015), the ranges of estimated reservoir temperatures for saline, cold, and hot springs are 65. 1ºC-109.0ºC, 37.8ºC-64.4ºC, and 65.5ºC-144.1ºC, respectively.…”
Section: Inference From Boron Isotopesmentioning
confidence: 99%
“…Several software, PHREEQC, MINTEQ, geochemists' workbench, can be used to calculate mass balance, saturated index, and model the reaction path, draw piper diagram, etc. By the process of water-rock interaction, major elements and TEs may be released and immigrate to other water bodies, therefore the major elements and trace element with distinguishing feature could be used as source apportionment [69,70]. However, the TEs undergo geochemical process of adsorption, desorption, mineralization, dissolution to change concentration in water.…”
Section: Geochemical Methodsmentioning
confidence: 99%