Titlebook: Geochemical Treasures and Petrogenetic Processes; John S. Armstrong-Altrin,Kailasa Pandarinath,Sanje Book 2022 The Editor(s) (if applicabl

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BORE

Identification and Modeling of Hydrogeochemical Processes in an Arid Zone of Mexican Highlandsof groundwater. The infiltration of water enriched with CO. reacts with albite and K feldspar, releasing silica, Na., K., Mg., and HCO. and the formation of clays. Reverse modeling indicates the formation of calcite, hematite, alteration of magnetite, and dissolution of gypsum.

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Boron Isotopic composition of Pegmatitic Tourmaline from Yumthang Valley, North Sikkim, Indiaotal REE and Type 2: having [(La/Yb). from (1.88 to 6.63)]. The δ.B values of the studied pegmatitic tourmalines are similar to that of the continental crust and S-type granites and ranges from − 13.83 ± 0.37 ‰ to − 12.78 ± 0.84 ‰ suggesting crustal origin. The low δ.B values from the studied tourma

含糊

Geochemistry and U–Pb CHIME Ages of Tonalite–Trondhjemitic–Granodioritic (TTG) Gneiss from the Centrent shows enriched nature, while HFS elements show depletion. Based on HREE concentration, the compiled TTG gneisses data from Central Bundelkhand terrane are further classified into three groups as low HREE (TTG-I), high HREE (TTG-II), and medium HREE (TTG-III). The protoliths of TTG gneisses are i

BOOST

The Geochemical Affinity of Paleogene Glauconites in Paleo-Tethyan Deposits of Indias show a wide variation in major oxide contents, viz. K.O (3.09–8.65 wt%), Fe.O. (15.33–29.49 wt%), Al.O. (5.12–16.77 wt%), MgO (2.06–9.00 wt%), and SiO. (39.16–57.02 wt%). The chemical composition of the glauconite, therefore, encompasses the entire range of K-poor to K-rich glauconite, supporting

fatty-acids

Paleoenvironmental Dynamics in a Mesoproterozoic Epicontinental Sea, Faded Shale, Son Valley, Indiain refractory elements, although both are now vertically juxtaposed in the same paleogeography. The majority of samples display MREE enrichment presumably because of organic matter (OM) abundance. The ST facies, apparently bears geochemical signature of the shallow shelf. Various paleoredox-sensitiv

outer-ear

Detrital Zircon Geochemistry in the Morita Formation, Northern Sonora, Mexico: Implications for Origcons show depleted LREE and very strongly enriched HREE patterns with positive Ce and negative Eu anomalies. The presence of significant negative Eu anomalies in these zircons suggest also that they were largely contributed by granitoids sources. Some zircons have relatively flat LREE and very stron