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Palabras clave – provistas por la editorial

preparation; hydroxysodalite; bentonite; alkali-activation; water-bath; total porosity; shale gas reservoir; Longmaxi Formation; Southeast Chongqing; pyrite; thermal treatment; pyrrhotite; Hg(II) removal; mechanism; Changling Fault Depression; Shahezi Formation; fractal dimensions; pore structure; shale lithofacies; lacustrine shales; pore networks; pore connectivity; spontaneous fluid imbibition; Shahezi shales; Sm–Nd dating; Shuiyindong; Carlin-type gold deposit; Southwestern China; southern North China; marine shale; nanopore structure; heterogeneity; fractal dimension; calcium carbonate; mesopore; amoxicillin; adsorption; kinetics; thermodynamics; nanocubic pyrite; hydrothermal synthesis; greigite; thiourea; iron; nanoparticle; Fe; nanomaterial; colloid; L-edge XANES; speciation; hierarchical nanocomposite; sepiolite; clay mineral; heavy metals; water treatment; nanograins; principal slip zone; crystallographic preferred orientation; amorphization; mirror-slip surface; faults; earthquakes; localization; Nantuo Formation; syn-glacial dolostone; rare earth elements; ferruginous conditions; South China; nanostructure; OM–clay aggregate; silica nanograin; tectonic and thermal evolution; Longmaxi Formation shale; N2 adsorption; helium ion microscope; minerals; trace elements; major elements; fault zone; tectonically deformed coal; differentiation mechanism; metallic nanoparticles; migration mechanism; prospecting; Shenjiayao gold deposit; syngenetic framboids; diagenetic framboids; paleoredox conditions; shale gas content; middle Yangtze area; nanocrystalline rutile; phase transition; metallization; high pressure; diamond anvil cell; n/a