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Non-Skeletal ComponentsMiocene outcrops, are calcitic (M., 1972). In some sediments lithoclasts may represent the major source of calcitic grains; for example, the carbonate-rich sediments leeward of Andros gain most of their calcite from land-derived lithoclasts.
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elevant to those working with modern carbonates but will also serve as a necessary reference source for those interested in ancient analogs. The first volume, by MILLIMAN, deals almost exclu sively with marine environments, while the second volume, by MULLER and FORST NER, will concentrate on the non-marine978-3-642-65530-2978-3-642-65528-9
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John D. Milliman,German Müller,Ulrich Förstnerer areas and K-12 grade levels. Although the focus of the text is science education, it should provide valuable reading for any individuals with interests in professional teacher education.978-1-4020-0275-5978-0-306-47217-6Series ISSN 1878-0482 Series E-ISSN 1878-0784
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