000			01991nam a2200121Ia 4500
008			220620s9999||||xx |||||||||||||| ||und||
245		0	_aNanomineralogy
546			_aEnglish[eng]
650			_apreparation||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
700			_aJu, Yiwen||Wan, Quan||Hochella, Jr.
856			_uhttps://mdpi.com/books/pdfview/book/2593
942			_cEB
999			_c25952 _d25952