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<article article-type="research-article">
<front>
<journal-meta>
<journal-id journal-id-type="archive">gsminmag</journal-id>
<journal-title>Mineralogical Magazine</journal-title>
<abbrev-journal-title abbrev-type="full">Mineralogical Magazine</abbrev-journal-title>
<issn pub-type="ppub">0026-461X</issn>
<publisher>
<publisher-name>Mineralogical Society</publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.1180/minmag.1994.058.390.12</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Petrology and Geochemistry</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>Diagenetic Volume-for-Volume Replacement: Force of Crystallization and Depression of Dissolution</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Minguez</surname>
<given-names>Jose Maria</given-names>
</name>
<aff>Departamento de Fisica Aplicada II, Universidad del Pa&#x00ED;s Vasco, 48080 Bilbao, Spain</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Elorza</surname>
<given-names>Javier</given-names>
</name>
<aff>Departamento de Mineralog&#x00ED;a y Petrolog&#x00ED;a, Universidad del Pa&#x00ED;s Vasco, 48080 Bilbao, Spain</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1994</year>
</pub-date>
<volume>58</volume>
<issue>390</issue>
<fpage>135</fpage>
<lpage>142</lpage>
<history>
<date date-type="received">
<day>8</day>
<month>3</month>
<year>1993</year>
</date>
<date date-type="rev-recd">
<day>30</day>
<month>4</month>
<year>1993</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1994, The Mineralogical Society</copyright-statement>
<copyright-year>1994</copyright-year>
<abstract>
<title>Abstract</title>
<p>The concept of force of crystallization is combined with that of depression of dissolution to explain diagenetic volume-for-volume replacement in both cases, either when the pressure is increased in early sedimentary settings, or when it is diminished in a late exposure. Also, a new textural criterion is added to the three classical ones in order to recognize diagenetic volume-for-volume replacement, and calculations are carried out to estimate the speed of the replacement.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>force of crystallization</kwd>
<kwd>volume-for-volume replacement</kwd>
<kwd>dissolution</kwd>
<kwd>diagenesis</kwd>
</kwd-group>
</article-meta>
</front>
</article>
