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ＣＡＳは、 １２１７３ ６０ ３ 、ＩＮＫＩは、 ＩＬＬＩＴＥ です. 一般的な堆積環境では、粘土鉱物はスメクタイトから始まり、 Ｉ Ｓ 混合層状鉱物過程を得て最終的にイライトに転移する。 Ｍ以下で雲母と似ていて底面間隔 Ｄ Ｓｐａｃｉｎｇ は、 10Å. K08-09(Al, Fe, Mg)2(Si, Al)4O10(OH)2. Ｃｈａｒｇｅ は、０１０ ＯＨ ２. しかし、最近の新しい分析技術を利用した分析結果によると、イライトの層電荷は、０１０ ＯＨ ２当 たり、０ ０以上まで上がるのも多いし特に、熱水変質イライトは、堆積環境下でスメクタイト由来のイライトの層電荷値よりより高かった Meunier と Velde, 1989; Srodon, 1992; Choo, 1996. が最も優勢で、 Ca2 , Mg2 , NH4. Ｄ値、すなわち、 d(001)=10 0.05. D(060)=1.50 0.01. ２ １八面体層は、結合構造内にある３つの陽イオンの場所のうち、２ヶ所のみ陽イオンになる二八面体 dioctahedral が特徴である。
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Universität Bern - Institut für Geologie
Institut für geologie. Arbeiten an der Uni. Institut für Geologie. Rund um die Geologie. Willkommen am Institut für Geologie. Wir begrüssen herzlich zwei neue Professoren am. Institut für Geologie:. Leitet die Forschungsgruppe Mineralogie. Und am Paul Scherrer Institut das Labor für Endlagersicherheit. Prof Jörg Hermann. Leitet die Forschungsgruppe Petrologie. Wir wünschen beiden einen guten Start! Postdoc in der Forschungsgruppe Paleozeanologie. Finden Sie Informationen wie Studiumnews. Das Masterstud...
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