Sedimentary Carbonate Minerals:
and their identification obviates individual thermochemical studies on every genus. The stability relations among sedimentary carbonate minerals are now more or less well known. The common rock-forming minerals cal cite and dolomite are indeed stable phases in the pertinent systems. Most other carbo...
Gespeichert in:
| 1. Verfasser: | |
|---|---|
| Format: | Elektronisch E-Book |
| Sprache: | English |
| Veröffentlicht: |
Berlin, Heidelberg
Springer Berlin Heidelberg
1973
|
| Schriftenreihe: | Minerals, Rocks and Inorganic Materials, Monograph Series of Theoretical and Experimental Studies
6 |
| Schlagworte: | |
| Online-Zugang: | BTU01 Volltext |
| Zusammenfassung: | and their identification obviates individual thermochemical studies on every genus. The stability relations among sedimentary carbonate minerals are now more or less well known. The common rock-forming minerals cal cite and dolomite are indeed stable phases in the pertinent systems. Most other carbonate minerals of similar composition which are known to occur in the younger sediments are metastable with respect to calcite, dolomite, and magnesite. This implies that the sedimentation of carbon ates is determined only in part by stability relations. Kinetic factors, which allow the formation of metastable minerals, appear to be more important. Although the diagenetic transformations leading to stable minerals take place by virtue of thermodynamic requirements, the reac tions themselves are triggered by kinetic factors as well. Some of the reactions leading from metastable to stable carbonate assemblages are susceptible to simulation in the laboratory; others (e. g. dolomitization) appear to be so slow that they can be studied only in analogous systems characterized by reasonable reaction rates. In all attempts to explain the possible mechanisms of such reactions, we must consider the crystal structures of the final products as well as of the starting materials. This is another viewpoint from which mineralogy is important to carbonate petrology, if we regard the crystal chemistry of minerals as a part of mineralogy. A certain parallelism with clay mineralogy suggests itself |
| Beschreibung: | 1 Online-Ressource (VI, 229 p) |
| ISBN: | 9783642654749 |
| DOI: | 10.1007/978-3-642-65474-9 |
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| 520 | |a and their identification obviates individual thermochemical studies on every genus. The stability relations among sedimentary carbonate minerals are now more or less well known. The common rock-forming minerals cal cite and dolomite are indeed stable phases in the pertinent systems. Most other carbonate minerals of similar composition which are known to occur in the younger sediments are metastable with respect to calcite, dolomite, and magnesite. This implies that the sedimentation of carbon ates is determined only in part by stability relations. Kinetic factors, which allow the formation of metastable minerals, appear to be more important. Although the diagenetic transformations leading to stable minerals take place by virtue of thermodynamic requirements, the reac tions themselves are triggered by kinetic factors as well. Some of the reactions leading from metastable to stable carbonate assemblages are susceptible to simulation in the laboratory; others (e. g. dolomitization) appear to be so slow that they can be studied only in analogous systems characterized by reasonable reaction rates. In all attempts to explain the possible mechanisms of such reactions, we must consider the crystal structures of the final products as well as of the starting materials. This is another viewpoint from which mineralogy is important to carbonate petrology, if we regard the crystal chemistry of minerals as a part of mineralogy. A certain parallelism with clay mineralogy suggests itself | ||
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Datensatz im Suchindex
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| any_adam_object | |
| author | Lippmann, Friedrich |
| author_facet | Lippmann, Friedrich |
| author_role | aut |
| author_sort | Lippmann, Friedrich |
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| building | Verbundindex |
| bvnumber | BV045177488 |
| collection | ZDB-2-EES |
| ctrlnum | (ZDB-2-EES)978-3-642-65474-9 (OCoLC)1184347216 (DE-599)BVBBV045177488 |
| dewey-full | 551.3 |
| dewey-hundreds | 500 - Natural sciences and mathematics |
| dewey-ones | 551 - Geology, hydrology, meteorology |
| dewey-raw | 551.3 |
| dewey-search | 551.3 |
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| dewey-tens | 550 - Earth sciences |
| discipline | Geologie / Paläontologie |
| doi_str_mv | 10.1007/978-3-642-65474-9 |
| format | Electronic eBook |
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| id | DE-604.BV045177488 |
| illustrated | Not Illustrated |
| indexdate | 2024-07-10T08:10:47Z |
| institution | BVB |
| isbn | 9783642654749 |
| language | English |
| oai_aleph_id | oai:aleph.bib-bvb.de:BVB01-030566717 |
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| physical | 1 Online-Ressource (VI, 229 p) |
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| publishDate | 1973 |
| publishDateSearch | 1973 |
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| publisher | Springer Berlin Heidelberg |
| record_format | marc |
| series2 | Minerals, Rocks and Inorganic Materials, Monograph Series of Theoretical and Experimental Studies |
| spelling | Lippmann, Friedrich Verfasser aut Sedimentary Carbonate Minerals by Friedrich Lippmann Berlin, Heidelberg Springer Berlin Heidelberg 1973 1 Online-Ressource (VI, 229 p) txt rdacontent c rdamedia cr rdacarrier Minerals, Rocks and Inorganic Materials, Monograph Series of Theoretical and Experimental Studies 6 and their identification obviates individual thermochemical studies on every genus. The stability relations among sedimentary carbonate minerals are now more or less well known. The common rock-forming minerals cal cite and dolomite are indeed stable phases in the pertinent systems. Most other carbonate minerals of similar composition which are known to occur in the younger sediments are metastable with respect to calcite, dolomite, and magnesite. This implies that the sedimentation of carbon ates is determined only in part by stability relations. Kinetic factors, which allow the formation of metastable minerals, appear to be more important. Although the diagenetic transformations leading to stable minerals take place by virtue of thermodynamic requirements, the reac tions themselves are triggered by kinetic factors as well. Some of the reactions leading from metastable to stable carbonate assemblages are susceptible to simulation in the laboratory; others (e. g. dolomitization) appear to be so slow that they can be studied only in analogous systems characterized by reasonable reaction rates. In all attempts to explain the possible mechanisms of such reactions, we must consider the crystal structures of the final products as well as of the starting materials. This is another viewpoint from which mineralogy is important to carbonate petrology, if we regard the crystal chemistry of minerals as a part of mineralogy. A certain parallelism with clay mineralogy suggests itself Earth Sciences Sedimentology Mineralogy Earth sciences Sediment (DE-588)4054079-0 gnd rswk-swf Carbonatgestein (DE-588)4147301-2 gnd rswk-swf Mineralogie (DE-588)4039457-8 gnd rswk-swf Carbonate (DE-588)4147300-0 gnd rswk-swf Carbonate (DE-588)4147300-0 s Mineralogie (DE-588)4039457-8 s 1\p DE-604 Sediment (DE-588)4054079-0 s Carbonatgestein (DE-588)4147301-2 s 2\p DE-604 Erscheint auch als Druck-Ausgabe 9783642654763 https://doi.org/10.1007/978-3-642-65474-9 Verlag URL des Erstveröffentlichers Volltext 1\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk 2\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk |
| spellingShingle | Lippmann, Friedrich Sedimentary Carbonate Minerals Earth Sciences Sedimentology Mineralogy Earth sciences Sediment (DE-588)4054079-0 gnd Carbonatgestein (DE-588)4147301-2 gnd Mineralogie (DE-588)4039457-8 gnd Carbonate (DE-588)4147300-0 gnd |
| subject_GND | (DE-588)4054079-0 (DE-588)4147301-2 (DE-588)4039457-8 (DE-588)4147300-0 |
| title | Sedimentary Carbonate Minerals |
| title_auth | Sedimentary Carbonate Minerals |
| title_exact_search | Sedimentary Carbonate Minerals |
| title_full | Sedimentary Carbonate Minerals by Friedrich Lippmann |
| title_fullStr | Sedimentary Carbonate Minerals by Friedrich Lippmann |
| title_full_unstemmed | Sedimentary Carbonate Minerals by Friedrich Lippmann |
| title_short | Sedimentary Carbonate Minerals |
| title_sort | sedimentary carbonate minerals |
| topic | Earth Sciences Sedimentology Mineralogy Earth sciences Sediment (DE-588)4054079-0 gnd Carbonatgestein (DE-588)4147301-2 gnd Mineralogie (DE-588)4039457-8 gnd Carbonate (DE-588)4147300-0 gnd |
| topic_facet | Earth Sciences Sedimentology Mineralogy Earth sciences Sediment Carbonatgestein Mineralogie Carbonate |
| url | https://doi.org/10.1007/978-3-642-65474-9 |
| work_keys_str_mv | AT lippmannfriedrich sedimentarycarbonateminerals |