Field Geology of High-Grade Gneiss Terrains:
Although there are numerous publications on the geology of high-grade gneiss terrains, few descriptions exist of how to map and carry out structural analysis in these terrains. Textbooks on structural geology concentrate on technIques appli cable to low-grade terrains. Geologists who have no experie...
Gespeichert in:
| Hauptverfasser: | , , |
|---|---|
| Format: | Elektronisch E-Book |
| Sprache: | English |
| Veröffentlicht: |
Berlin, Heidelberg
Springer Berlin Heidelberg
1990
|
| Schlagworte: | |
| Online-Zugang: | BTU01 Volltext |
| Zusammenfassung: | Although there are numerous publications on the geology of high-grade gneiss terrains, few descriptions exist of how to map and carry out structural analysis in these terrains. Textbooks on structural geology concentrate on technIques appli cable to low-grade terrains. Geologists who have no experience of mapping high-grade gneisses are often at a loss as to how to apply techniques to high grade rocks that were developed for low to medium grade metamorphic terrains. Any study of deep crustal processes and their development through time should begin with examination of the primary data source - outcrops of high grade metamorphic terrains. We feel that the urge to apply advanced techniques of fabric analysis, petrology, geochemistry, isotope geochemistry and age deter mination to these rocks often results in brief sampling trips in which there is little, if any analysis of the structural and metamorphic history revealed by outcrop patterns. Many studies of the metamorphic petrology and geochemistry of high-grade gneiss terrains make ineffective use of available field data, often because the authors are unaware of structural complexities and of the ways to recognise and use them. This is unfortunate, because much data can be collected in the field at minimal cost that cannot easily, if at all, be obtained from material in the laboratory. The primary igneous or sedimentary nature of a rock, the relative age of intrusive veins, and the sequence of deformation that they under went, can usually best be determined by straightforward observation in the field |
| Beschreibung: | 1 Online-Ressource (IX, 150 p. 57 illus) |
| ISBN: | 9783642760136 |
| DOI: | 10.1007/978-3-642-76013-6 |
Internformat
MARC
| LEADER | 00000nmm a2200000zc 4500 | ||
|---|---|---|---|
| 001 | BV045178125 | ||
| 003 | DE-604 | ||
| 005 | 00000000000000.0 | ||
| 007 | cr|uuu---uuuuu | ||
| 008 | 180911s1990 |||| o||u| ||||||eng d | ||
| 020 | |a 9783642760136 |9 978-3-642-76013-6 | ||
| 024 | 7 | |a 10.1007/978-3-642-76013-6 |2 doi | |
| 035 | |a (ZDB-2-EES)978-3-642-76013-6 | ||
| 035 | |a (OCoLC)1053814349 | ||
| 035 | |a (DE-599)BVBBV045178125 | ||
| 040 | |a DE-604 |b ger |e aacr | ||
| 041 | 0 | |a eng | |
| 049 | |a DE-634 | ||
| 082 | 0 | |a 551 |2 23 | |
| 084 | |a RB 10121 |0 (DE-625)142220:12623 |2 rvk | ||
| 084 | |a TZ 5000 |0 (DE-625)145138: |2 rvk | ||
| 084 | |a TG 1100 |0 (DE-625)143863: |2 rvk | ||
| 084 | |a TH 2450 |0 (DE-625)163676: |2 rvk | ||
| 100 | 1 | |a Passchier, Cees W. |e Verfasser |4 aut | |
| 245 | 1 | 0 | |a Field Geology of High-Grade Gneiss Terrains |c by Cees W. Passchier, John Stuart Myers, Alfred Krner |
| 264 | 1 | |a Berlin, Heidelberg |b Springer Berlin Heidelberg |c 1990 | |
| 300 | |a 1 Online-Ressource (IX, 150 p. 57 illus) | ||
| 336 | |b txt |2 rdacontent | ||
| 337 | |b c |2 rdamedia | ||
| 338 | |b cr |2 rdacarrier | ||
| 520 | |a Although there are numerous publications on the geology of high-grade gneiss terrains, few descriptions exist of how to map and carry out structural analysis in these terrains. Textbooks on structural geology concentrate on technIques appli cable to low-grade terrains. Geologists who have no experience of mapping high-grade gneisses are often at a loss as to how to apply techniques to high grade rocks that were developed for low to medium grade metamorphic terrains. Any study of deep crustal processes and their development through time should begin with examination of the primary data source - outcrops of high grade metamorphic terrains. We feel that the urge to apply advanced techniques of fabric analysis, petrology, geochemistry, isotope geochemistry and age deter mination to these rocks often results in brief sampling trips in which there is little, if any analysis of the structural and metamorphic history revealed by outcrop patterns. Many studies of the metamorphic petrology and geochemistry of high-grade gneiss terrains make ineffective use of available field data, often because the authors are unaware of structural complexities and of the ways to recognise and use them. This is unfortunate, because much data can be collected in the field at minimal cost that cannot easily, if at all, be obtained from material in the laboratory. The primary igneous or sedimentary nature of a rock, the relative age of intrusive veins, and the sequence of deformation that they under went, can usually best be determined by straightforward observation in the field | ||
| 650 | 4 | |a Earth Sciences | |
| 650 | 4 | |a Geology | |
| 650 | 4 | |a Geochemistry | |
| 650 | 4 | |a Mineralogy | |
| 650 | 4 | |a Earth sciences | |
| 650 | 4 | |a Geochemistry | |
| 650 | 4 | |a Geology | |
| 650 | 4 | |a Mineralogy | |
| 650 | 0 | 7 | |a Gefügekunde |0 (DE-588)4125137-4 |2 gnd |9 rswk-swf |
| 650 | 0 | 7 | |a Gneis |0 (DE-588)4130378-7 |2 gnd |9 rswk-swf |
| 650 | 0 | 7 | |a Feldgeologie |0 (DE-588)4153918-7 |2 gnd |9 rswk-swf |
| 689 | 0 | 0 | |a Gneis |0 (DE-588)4130378-7 |D s |
| 689 | 0 | 1 | |a Feldgeologie |0 (DE-588)4153918-7 |D s |
| 689 | 0 | |8 1\p |5 DE-604 | |
| 689 | 1 | 0 | |a Gneis |0 (DE-588)4130378-7 |D s |
| 689 | 1 | 1 | |a Gefügekunde |0 (DE-588)4125137-4 |D s |
| 689 | 1 | |8 2\p |5 DE-604 | |
| 700 | 1 | |a Myers, John Stuart |4 aut | |
| 700 | 1 | |a Krner, Alfred |4 aut | |
| 776 | 0 | 8 | |i Erscheint auch als |n Druck-Ausgabe |z 9783540530534 |
| 856 | 4 | 0 | |u https://doi.org/10.1007/978-3-642-76013-6 |x Verlag |z URL des Erstveröffentlichers |3 Volltext |
| 912 | |a ZDB-2-EES | ||
| 940 | 1 | |q ZDB-2-EES_Archiv | |
| 999 | |a oai:aleph.bib-bvb.de:BVB01-030567355 | ||
| 883 | 1 | |8 1\p |a cgwrk |d 20201028 |q DE-101 |u https://d-nb.info/provenance/plan#cgwrk | |
| 883 | 1 | |8 2\p |a cgwrk |d 20201028 |q DE-101 |u https://d-nb.info/provenance/plan#cgwrk | |
| 966 | e | |u https://doi.org/10.1007/978-3-642-76013-6 |l BTU01 |p ZDB-2-EES |q ZDB-2-EES_Archiv |x Verlag |3 Volltext | |
Datensatz im Suchindex
| _version_ | 1804178867984793600 |
|---|---|
| any_adam_object | |
| author | Passchier, Cees W. Myers, John Stuart Krner, Alfred |
| author_facet | Passchier, Cees W. Myers, John Stuart Krner, Alfred |
| author_role | aut aut aut |
| author_sort | Passchier, Cees W. |
| author_variant | c w p cw cwp j s m js jsm a k ak |
| building | Verbundindex |
| bvnumber | BV045178125 |
| classification_rvk | RB 10121 TZ 5000 TG 1100 TH 2450 |
| collection | ZDB-2-EES |
| ctrlnum | (ZDB-2-EES)978-3-642-76013-6 (OCoLC)1053814349 (DE-599)BVBBV045178125 |
| dewey-full | 551 |
| dewey-hundreds | 500 - Natural sciences and mathematics |
| dewey-ones | 551 - Geology, hydrology, meteorology |
| dewey-raw | 551 |
| dewey-search | 551 |
| dewey-sort | 3551 |
| dewey-tens | 550 - Earth sciences |
| discipline | Geologie / Paläontologie Geographie |
| doi_str_mv | 10.1007/978-3-642-76013-6 |
| format | Electronic eBook |
| fullrecord | <?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>03951nmm a2200661zc 4500</leader><controlfield tag="001">BV045178125</controlfield><controlfield tag="003">DE-604</controlfield><controlfield tag="005">00000000000000.0</controlfield><controlfield tag="007">cr|uuu---uuuuu</controlfield><controlfield tag="008">180911s1990 |||| o||u| ||||||eng d</controlfield><datafield tag="020" ind1=" " ind2=" "><subfield code="a">9783642760136</subfield><subfield code="9">978-3-642-76013-6</subfield></datafield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/978-3-642-76013-6</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ZDB-2-EES)978-3-642-76013-6</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(OCoLC)1053814349</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)BVBBV045178125</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-604</subfield><subfield code="b">ger</subfield><subfield code="e">aacr</subfield></datafield><datafield tag="041" ind1="0" ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="049" ind1=" " ind2=" "><subfield code="a">DE-634</subfield></datafield><datafield tag="082" ind1="0" ind2=" "><subfield code="a">551</subfield><subfield code="2">23</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">RB 10121</subfield><subfield code="0">(DE-625)142220:12623</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">TZ 5000</subfield><subfield code="0">(DE-625)145138:</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">TG 1100</subfield><subfield code="0">(DE-625)143863:</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">TH 2450</subfield><subfield code="0">(DE-625)163676:</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Passchier, Cees W.</subfield><subfield code="e">Verfasser</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Field Geology of High-Grade Gneiss Terrains</subfield><subfield code="c">by Cees W. Passchier, John Stuart Myers, Alfred Krner</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Berlin, Heidelberg</subfield><subfield code="b">Springer Berlin Heidelberg</subfield><subfield code="c">1990</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">1 Online-Ressource (IX, 150 p. 57 illus)</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Although there are numerous publications on the geology of high-grade gneiss terrains, few descriptions exist of how to map and carry out structural analysis in these terrains. Textbooks on structural geology concentrate on technIques appli cable to low-grade terrains. Geologists who have no experience of mapping high-grade gneisses are often at a loss as to how to apply techniques to high grade rocks that were developed for low to medium grade metamorphic terrains. Any study of deep crustal processes and their development through time should begin with examination of the primary data source - outcrops of high grade metamorphic terrains. We feel that the urge to apply advanced techniques of fabric analysis, petrology, geochemistry, isotope geochemistry and age deter mination to these rocks often results in brief sampling trips in which there is little, if any analysis of the structural and metamorphic history revealed by outcrop patterns. Many studies of the metamorphic petrology and geochemistry of high-grade gneiss terrains make ineffective use of available field data, often because the authors are unaware of structural complexities and of the ways to recognise and use them. This is unfortunate, because much data can be collected in the field at minimal cost that cannot easily, if at all, be obtained from material in the laboratory. The primary igneous or sedimentary nature of a rock, the relative age of intrusive veins, and the sequence of deformation that they under went, can usually best be determined by straightforward observation in the field</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Earth Sciences</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geology</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geochemistry</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Mineralogy</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Earth sciences</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geochemistry</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geology</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Mineralogy</subfield></datafield><datafield tag="650" ind1="0" ind2="7"><subfield code="a">Gefügekunde</subfield><subfield code="0">(DE-588)4125137-4</subfield><subfield code="2">gnd</subfield><subfield code="9">rswk-swf</subfield></datafield><datafield tag="650" ind1="0" ind2="7"><subfield code="a">Gneis</subfield><subfield code="0">(DE-588)4130378-7</subfield><subfield code="2">gnd</subfield><subfield code="9">rswk-swf</subfield></datafield><datafield tag="650" ind1="0" ind2="7"><subfield code="a">Feldgeologie</subfield><subfield code="0">(DE-588)4153918-7</subfield><subfield code="2">gnd</subfield><subfield code="9">rswk-swf</subfield></datafield><datafield tag="689" ind1="0" ind2="0"><subfield code="a">Gneis</subfield><subfield code="0">(DE-588)4130378-7</subfield><subfield code="D">s</subfield></datafield><datafield tag="689" ind1="0" ind2="1"><subfield code="a">Feldgeologie</subfield><subfield code="0">(DE-588)4153918-7</subfield><subfield code="D">s</subfield></datafield><datafield tag="689" ind1="0" ind2=" "><subfield code="8">1\p</subfield><subfield code="5">DE-604</subfield></datafield><datafield tag="689" ind1="1" ind2="0"><subfield code="a">Gneis</subfield><subfield code="0">(DE-588)4130378-7</subfield><subfield code="D">s</subfield></datafield><datafield tag="689" ind1="1" ind2="1"><subfield code="a">Gefügekunde</subfield><subfield code="0">(DE-588)4125137-4</subfield><subfield code="D">s</subfield></datafield><datafield tag="689" ind1="1" ind2=" "><subfield code="8">2\p</subfield><subfield code="5">DE-604</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Myers, John Stuart</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Krner, Alfred</subfield><subfield code="4">aut</subfield></datafield><datafield tag="776" ind1="0" ind2="8"><subfield code="i">Erscheint auch als</subfield><subfield code="n">Druck-Ausgabe</subfield><subfield code="z">9783540530534</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1007/978-3-642-76013-6</subfield><subfield code="x">Verlag</subfield><subfield code="z">URL des Erstveröffentlichers</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ZDB-2-EES</subfield></datafield><datafield tag="940" ind1="1" ind2=" "><subfield code="q">ZDB-2-EES_Archiv</subfield></datafield><datafield tag="999" ind1=" " ind2=" "><subfield code="a">oai:aleph.bib-bvb.de:BVB01-030567355</subfield></datafield><datafield tag="883" ind1="1" ind2=" "><subfield code="8">1\p</subfield><subfield code="a">cgwrk</subfield><subfield code="d">20201028</subfield><subfield code="q">DE-101</subfield><subfield code="u">https://d-nb.info/provenance/plan#cgwrk</subfield></datafield><datafield tag="883" ind1="1" ind2=" "><subfield code="8">2\p</subfield><subfield code="a">cgwrk</subfield><subfield code="d">20201028</subfield><subfield code="q">DE-101</subfield><subfield code="u">https://d-nb.info/provenance/plan#cgwrk</subfield></datafield><datafield tag="966" ind1="e" ind2=" "><subfield code="u">https://doi.org/10.1007/978-3-642-76013-6</subfield><subfield code="l">BTU01</subfield><subfield code="p">ZDB-2-EES</subfield><subfield code="q">ZDB-2-EES_Archiv</subfield><subfield code="x">Verlag</subfield><subfield code="3">Volltext</subfield></datafield></record></collection> |
| id | DE-604.BV045178125 |
| illustrated | Not Illustrated |
| indexdate | 2024-07-10T08:10:48Z |
| institution | BVB |
| isbn | 9783642760136 |
| language | English |
| oai_aleph_id | oai:aleph.bib-bvb.de:BVB01-030567355 |
| oclc_num | 1053814349 |
| open_access_boolean | |
| owner | DE-634 |
| owner_facet | DE-634 |
| physical | 1 Online-Ressource (IX, 150 p. 57 illus) |
| psigel | ZDB-2-EES ZDB-2-EES_Archiv ZDB-2-EES ZDB-2-EES_Archiv |
| publishDate | 1990 |
| publishDateSearch | 1990 |
| publishDateSort | 1990 |
| publisher | Springer Berlin Heidelberg |
| record_format | marc |
| spelling | Passchier, Cees W. Verfasser aut Field Geology of High-Grade Gneiss Terrains by Cees W. Passchier, John Stuart Myers, Alfred Krner Berlin, Heidelberg Springer Berlin Heidelberg 1990 1 Online-Ressource (IX, 150 p. 57 illus) txt rdacontent c rdamedia cr rdacarrier Although there are numerous publications on the geology of high-grade gneiss terrains, few descriptions exist of how to map and carry out structural analysis in these terrains. Textbooks on structural geology concentrate on technIques appli cable to low-grade terrains. Geologists who have no experience of mapping high-grade gneisses are often at a loss as to how to apply techniques to high grade rocks that were developed for low to medium grade metamorphic terrains. Any study of deep crustal processes and their development through time should begin with examination of the primary data source - outcrops of high grade metamorphic terrains. We feel that the urge to apply advanced techniques of fabric analysis, petrology, geochemistry, isotope geochemistry and age deter mination to these rocks often results in brief sampling trips in which there is little, if any analysis of the structural and metamorphic history revealed by outcrop patterns. Many studies of the metamorphic petrology and geochemistry of high-grade gneiss terrains make ineffective use of available field data, often because the authors are unaware of structural complexities and of the ways to recognise and use them. This is unfortunate, because much data can be collected in the field at minimal cost that cannot easily, if at all, be obtained from material in the laboratory. The primary igneous or sedimentary nature of a rock, the relative age of intrusive veins, and the sequence of deformation that they under went, can usually best be determined by straightforward observation in the field Earth Sciences Geology Geochemistry Mineralogy Earth sciences Gefügekunde (DE-588)4125137-4 gnd rswk-swf Gneis (DE-588)4130378-7 gnd rswk-swf Feldgeologie (DE-588)4153918-7 gnd rswk-swf Gneis (DE-588)4130378-7 s Feldgeologie (DE-588)4153918-7 s 1\p DE-604 Gefügekunde (DE-588)4125137-4 s 2\p DE-604 Myers, John Stuart aut Krner, Alfred aut Erscheint auch als Druck-Ausgabe 9783540530534 https://doi.org/10.1007/978-3-642-76013-6 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 | Passchier, Cees W. Myers, John Stuart Krner, Alfred Field Geology of High-Grade Gneiss Terrains Earth Sciences Geology Geochemistry Mineralogy Earth sciences Gefügekunde (DE-588)4125137-4 gnd Gneis (DE-588)4130378-7 gnd Feldgeologie (DE-588)4153918-7 gnd |
| subject_GND | (DE-588)4125137-4 (DE-588)4130378-7 (DE-588)4153918-7 |
| title | Field Geology of High-Grade Gneiss Terrains |
| title_auth | Field Geology of High-Grade Gneiss Terrains |
| title_exact_search | Field Geology of High-Grade Gneiss Terrains |
| title_full | Field Geology of High-Grade Gneiss Terrains by Cees W. Passchier, John Stuart Myers, Alfred Krner |
| title_fullStr | Field Geology of High-Grade Gneiss Terrains by Cees W. Passchier, John Stuart Myers, Alfred Krner |
| title_full_unstemmed | Field Geology of High-Grade Gneiss Terrains by Cees W. Passchier, John Stuart Myers, Alfred Krner |
| title_short | Field Geology of High-Grade Gneiss Terrains |
| title_sort | field geology of high grade gneiss terrains |
| topic | Earth Sciences Geology Geochemistry Mineralogy Earth sciences Gefügekunde (DE-588)4125137-4 gnd Gneis (DE-588)4130378-7 gnd Feldgeologie (DE-588)4153918-7 gnd |
| topic_facet | Earth Sciences Geology Geochemistry Mineralogy Earth sciences Gefügekunde Gneis Feldgeologie |
| url | https://doi.org/10.1007/978-3-642-76013-6 |
| work_keys_str_mv | AT passchierceesw fieldgeologyofhighgradegneissterrains AT myersjohnstuart fieldgeologyofhighgradegneissterrains AT krneralfred fieldgeologyofhighgradegneissterrains |