Cataclastic rheology of carbonate rocks
Abstract Based on the knowledge of the shallow-level mylonitization of detrital rocks and intrusive rocks, the poorly-known cataclastic rheology of carbonate rocks is discussed comprehensively in this paper. The cases taken from eastern China are analyzed in various aspects including ductile-brittle...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Lu, Xiancai [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2005 |
|---|
| Schlagwörter: |
|---|
| Anmerkung: |
© Science in China Press 2005 |
|---|
| Übergeordnetes Werk: |
Enthalten in: Science in China / D - Science in China Press, 1996, 48(2005), 8 vom: Aug., Seite 1227-1233 |
|---|---|
| Übergeordnetes Werk: |
volume:48 ; year:2005 ; number:8 ; month:08 ; pages:1227-1233 |
| Links: |
|---|
| DOI / URN: |
10.1360/04yd0085 |
|---|
| Katalog-ID: |
OLC2063777977 |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | OLC2063777977 | ||
| 003 | DE-627 | ||
| 005 | 20230504094349.0 | ||
| 007 | tu | ||
| 008 | 200820s2005 xx ||||| 00| ||eng c | ||
| 024 | 7 | |a 10.1360/04yd0085 |2 doi | |
| 035 | |a (DE-627)OLC2063777977 | ||
| 035 | |a (DE-He213)04yd0085-p | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | 4 | |a 550 |q VZ |
| 082 | 0 | 4 | |a 550 |q VZ |
| 084 | |a 13 |2 ssgn | ||
| 100 | 1 | |a Lu, Xiancai |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Cataclastic rheology of carbonate rocks |
| 264 | 1 | |c 2005 | |
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
| 338 | |a Band |b nc |2 rdacarrier | ||
| 500 | |a © Science in China Press 2005 | ||
| 520 | |a Abstract Based on the knowledge of the shallow-level mylonitization of detrital rocks and intrusive rocks, the poorly-known cataclastic rheology of carbonate rocks is discussed comprehensively in this paper. The cases taken from eastern China are analyzed in various aspects including ductile-brittle fault zone, rock texture and structure, clastomylonite layer, leucocratic stress minerals, and frictional dynamometamorphism. It is proposed that the cataclastic flow structure represented by clastomylonite texture is a cooling pattern of flow assemblage characterized by cooling metamorphism, cooling mylonite and cooling stress minerals. Such a pattern is formed generally in mildly reducing physicochemical environments, and is commonly related to regional tectonism and mesothermal and epithermal mineralization. | ||
| 650 | 4 | |a carbonate rock | |
| 650 | 4 | |a cataclastic rheology | |
| 650 | 4 | |a clastomylonite | |
| 650 | 4 | |a ductile-brittle fault zone | |
| 700 | 1 | |a Sun, Yan |4 aut | |
| 700 | 1 | |a Shu, Liangshu |4 aut | |
| 700 | 1 | |a Gu, Lianxing |4 aut | |
| 700 | 1 | |a Guo, Jichun |4 aut | |
| 700 | 1 | |a Zhu, Wenbin |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Science in China / D |d Science in China Press, 1996 |g 48(2005), 8 vom: Aug., Seite 1227-1233 |w (DE-627)193118238 |w (DE-600)1307899-9 |w (DE-576)062316923 |x 1006-9313 |7 nnns |
| 773 | 1 | 8 | |g volume:48 |g year:2005 |g number:8 |g month:08 |g pages:1227-1233 |
| 856 | 4 | 1 | |u https://doi.org/10.1360/04yd0085 |z lizenzpflichtig |3 Volltext |
| 912 | |a GBV_USEFLAG_A | ||
| 912 | |a SYSFLAG_A | ||
| 912 | |a GBV_OLC | ||
| 912 | |a SSG-OLC-OAS | ||
| 912 | |a SSG-OLC-MFO | ||
| 912 | |a SSG-OPC-GGO | ||
| 912 | |a GBV_ILN_22 | ||
| 912 | |a GBV_ILN_40 | ||
| 912 | |a GBV_ILN_70 | ||
| 912 | |a GBV_ILN_4082 | ||
| 951 | |a AR | ||
| 952 | |d 48 |j 2005 |e 8 |c 08 |h 1227-1233 | ||
| author_variant |
x l xl y s ys l s ls l g lg j g jg w z wz |
|---|---|
| matchkey_str |
article:10069313:2005----::aalsirelgocr |
| hierarchy_sort_str |
2005 |
| publishDate |
2005 |
| allfields |
10.1360/04yd0085 doi (DE-627)OLC2063777977 (DE-He213)04yd0085-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Lu, Xiancai verfasserin aut Cataclastic rheology of carbonate rocks 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 2005 Abstract Based on the knowledge of the shallow-level mylonitization of detrital rocks and intrusive rocks, the poorly-known cataclastic rheology of carbonate rocks is discussed comprehensively in this paper. The cases taken from eastern China are analyzed in various aspects including ductile-brittle fault zone, rock texture and structure, clastomylonite layer, leucocratic stress minerals, and frictional dynamometamorphism. It is proposed that the cataclastic flow structure represented by clastomylonite texture is a cooling pattern of flow assemblage characterized by cooling metamorphism, cooling mylonite and cooling stress minerals. Such a pattern is formed generally in mildly reducing physicochemical environments, and is commonly related to regional tectonism and mesothermal and epithermal mineralization. carbonate rock cataclastic rheology clastomylonite ductile-brittle fault zone Sun, Yan aut Shu, Liangshu aut Gu, Lianxing aut Guo, Jichun aut Zhu, Wenbin aut Enthalten in Science in China / D Science in China Press, 1996 48(2005), 8 vom: Aug., Seite 1227-1233 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:48 year:2005 number:8 month:08 pages:1227-1233 https://doi.org/10.1360/04yd0085 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_4082 AR 48 2005 8 08 1227-1233 |
| spelling |
10.1360/04yd0085 doi (DE-627)OLC2063777977 (DE-He213)04yd0085-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Lu, Xiancai verfasserin aut Cataclastic rheology of carbonate rocks 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 2005 Abstract Based on the knowledge of the shallow-level mylonitization of detrital rocks and intrusive rocks, the poorly-known cataclastic rheology of carbonate rocks is discussed comprehensively in this paper. The cases taken from eastern China are analyzed in various aspects including ductile-brittle fault zone, rock texture and structure, clastomylonite layer, leucocratic stress minerals, and frictional dynamometamorphism. It is proposed that the cataclastic flow structure represented by clastomylonite texture is a cooling pattern of flow assemblage characterized by cooling metamorphism, cooling mylonite and cooling stress minerals. Such a pattern is formed generally in mildly reducing physicochemical environments, and is commonly related to regional tectonism and mesothermal and epithermal mineralization. carbonate rock cataclastic rheology clastomylonite ductile-brittle fault zone Sun, Yan aut Shu, Liangshu aut Gu, Lianxing aut Guo, Jichun aut Zhu, Wenbin aut Enthalten in Science in China / D Science in China Press, 1996 48(2005), 8 vom: Aug., Seite 1227-1233 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:48 year:2005 number:8 month:08 pages:1227-1233 https://doi.org/10.1360/04yd0085 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_4082 AR 48 2005 8 08 1227-1233 |
| allfields_unstemmed |
10.1360/04yd0085 doi (DE-627)OLC2063777977 (DE-He213)04yd0085-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Lu, Xiancai verfasserin aut Cataclastic rheology of carbonate rocks 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 2005 Abstract Based on the knowledge of the shallow-level mylonitization of detrital rocks and intrusive rocks, the poorly-known cataclastic rheology of carbonate rocks is discussed comprehensively in this paper. The cases taken from eastern China are analyzed in various aspects including ductile-brittle fault zone, rock texture and structure, clastomylonite layer, leucocratic stress minerals, and frictional dynamometamorphism. It is proposed that the cataclastic flow structure represented by clastomylonite texture is a cooling pattern of flow assemblage characterized by cooling metamorphism, cooling mylonite and cooling stress minerals. Such a pattern is formed generally in mildly reducing physicochemical environments, and is commonly related to regional tectonism and mesothermal and epithermal mineralization. carbonate rock cataclastic rheology clastomylonite ductile-brittle fault zone Sun, Yan aut Shu, Liangshu aut Gu, Lianxing aut Guo, Jichun aut Zhu, Wenbin aut Enthalten in Science in China / D Science in China Press, 1996 48(2005), 8 vom: Aug., Seite 1227-1233 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:48 year:2005 number:8 month:08 pages:1227-1233 https://doi.org/10.1360/04yd0085 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_4082 AR 48 2005 8 08 1227-1233 |
| allfieldsGer |
10.1360/04yd0085 doi (DE-627)OLC2063777977 (DE-He213)04yd0085-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Lu, Xiancai verfasserin aut Cataclastic rheology of carbonate rocks 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 2005 Abstract Based on the knowledge of the shallow-level mylonitization of detrital rocks and intrusive rocks, the poorly-known cataclastic rheology of carbonate rocks is discussed comprehensively in this paper. The cases taken from eastern China are analyzed in various aspects including ductile-brittle fault zone, rock texture and structure, clastomylonite layer, leucocratic stress minerals, and frictional dynamometamorphism. It is proposed that the cataclastic flow structure represented by clastomylonite texture is a cooling pattern of flow assemblage characterized by cooling metamorphism, cooling mylonite and cooling stress minerals. Such a pattern is formed generally in mildly reducing physicochemical environments, and is commonly related to regional tectonism and mesothermal and epithermal mineralization. carbonate rock cataclastic rheology clastomylonite ductile-brittle fault zone Sun, Yan aut Shu, Liangshu aut Gu, Lianxing aut Guo, Jichun aut Zhu, Wenbin aut Enthalten in Science in China / D Science in China Press, 1996 48(2005), 8 vom: Aug., Seite 1227-1233 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:48 year:2005 number:8 month:08 pages:1227-1233 https://doi.org/10.1360/04yd0085 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_4082 AR 48 2005 8 08 1227-1233 |
| allfieldsSound |
10.1360/04yd0085 doi (DE-627)OLC2063777977 (DE-He213)04yd0085-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Lu, Xiancai verfasserin aut Cataclastic rheology of carbonate rocks 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 2005 Abstract Based on the knowledge of the shallow-level mylonitization of detrital rocks and intrusive rocks, the poorly-known cataclastic rheology of carbonate rocks is discussed comprehensively in this paper. The cases taken from eastern China are analyzed in various aspects including ductile-brittle fault zone, rock texture and structure, clastomylonite layer, leucocratic stress minerals, and frictional dynamometamorphism. It is proposed that the cataclastic flow structure represented by clastomylonite texture is a cooling pattern of flow assemblage characterized by cooling metamorphism, cooling mylonite and cooling stress minerals. Such a pattern is formed generally in mildly reducing physicochemical environments, and is commonly related to regional tectonism and mesothermal and epithermal mineralization. carbonate rock cataclastic rheology clastomylonite ductile-brittle fault zone Sun, Yan aut Shu, Liangshu aut Gu, Lianxing aut Guo, Jichun aut Zhu, Wenbin aut Enthalten in Science in China / D Science in China Press, 1996 48(2005), 8 vom: Aug., Seite 1227-1233 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:48 year:2005 number:8 month:08 pages:1227-1233 https://doi.org/10.1360/04yd0085 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_4082 AR 48 2005 8 08 1227-1233 |
| language |
English |
| source |
Enthalten in Science in China / D 48(2005), 8 vom: Aug., Seite 1227-1233 volume:48 year:2005 number:8 month:08 pages:1227-1233 |
| sourceStr |
Enthalten in Science in China / D 48(2005), 8 vom: Aug., Seite 1227-1233 volume:48 year:2005 number:8 month:08 pages:1227-1233 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
carbonate rock cataclastic rheology clastomylonite ductile-brittle fault zone |
| dewey-raw |
550 |
| isfreeaccess_bool |
false |
| container_title |
Science in China / D |
| authorswithroles_txt_mv |
Lu, Xiancai @@aut@@ Sun, Yan @@aut@@ Shu, Liangshu @@aut@@ Gu, Lianxing @@aut@@ Guo, Jichun @@aut@@ Zhu, Wenbin @@aut@@ |
| publishDateDaySort_date |
2005-08-01T00:00:00Z |
| hierarchy_top_id |
193118238 |
| dewey-sort |
3550 |
| id |
OLC2063777977 |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2063777977</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230504094349.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200820s2005 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1360/04yd0085</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2063777977</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)04yd0085-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Lu, Xiancai</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Cataclastic rheology of carbonate rocks</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2005</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Science in China Press 2005</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Based on the knowledge of the shallow-level mylonitization of detrital rocks and intrusive rocks, the poorly-known cataclastic rheology of carbonate rocks is discussed comprehensively in this paper. The cases taken from eastern China are analyzed in various aspects including ductile-brittle fault zone, rock texture and structure, clastomylonite layer, leucocratic stress minerals, and frictional dynamometamorphism. It is proposed that the cataclastic flow structure represented by clastomylonite texture is a cooling pattern of flow assemblage characterized by cooling metamorphism, cooling mylonite and cooling stress minerals. Such a pattern is formed generally in mildly reducing physicochemical environments, and is commonly related to regional tectonism and mesothermal and epithermal mineralization.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">carbonate rock</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">cataclastic rheology</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">clastomylonite</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">ductile-brittle fault zone</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Sun, Yan</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Shu, Liangshu</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Gu, Lianxing</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Guo, Jichun</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhu, Wenbin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Science in China / D</subfield><subfield code="d">Science in China Press, 1996</subfield><subfield code="g">48(2005), 8 vom: Aug., Seite 1227-1233</subfield><subfield code="w">(DE-627)193118238</subfield><subfield code="w">(DE-600)1307899-9</subfield><subfield code="w">(DE-576)062316923</subfield><subfield code="x">1006-9313</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:48</subfield><subfield code="g">year:2005</subfield><subfield code="g">number:8</subfield><subfield code="g">month:08</subfield><subfield code="g">pages:1227-1233</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1360/04yd0085</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-OAS</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-MFO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4082</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">48</subfield><subfield code="j">2005</subfield><subfield code="e">8</subfield><subfield code="c">08</subfield><subfield code="h">1227-1233</subfield></datafield></record></collection>
|
| author |
Lu, Xiancai |
| spellingShingle |
Lu, Xiancai ddc 550 ssgn 13 misc carbonate rock misc cataclastic rheology misc clastomylonite misc ductile-brittle fault zone Cataclastic rheology of carbonate rocks |
| authorStr |
Lu, Xiancai |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)193118238 |
| format |
Article |
| dewey-ones |
550 - Earth sciences |
| delete_txt_mv |
keep |
| author_role |
aut aut aut aut aut aut |
| collection |
OLC |
| remote_str |
false |
| illustrated |
Not Illustrated |
| issn |
1006-9313 |
| topic_title |
550 VZ 13 ssgn Cataclastic rheology of carbonate rocks carbonate rock cataclastic rheology clastomylonite ductile-brittle fault zone |
| topic |
ddc 550 ssgn 13 misc carbonate rock misc cataclastic rheology misc clastomylonite misc ductile-brittle fault zone |
| topic_unstemmed |
ddc 550 ssgn 13 misc carbonate rock misc cataclastic rheology misc clastomylonite misc ductile-brittle fault zone |
| topic_browse |
ddc 550 ssgn 13 misc carbonate rock misc cataclastic rheology misc clastomylonite misc ductile-brittle fault zone |
| format_facet |
Aufsätze Gedruckte Aufsätze |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
nc |
| hierarchy_parent_title |
Science in China / D |
| hierarchy_parent_id |
193118238 |
| dewey-tens |
550 - Earth sciences & geology |
| hierarchy_top_title |
Science in China / D |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 |
| title |
Cataclastic rheology of carbonate rocks |
| ctrlnum |
(DE-627)OLC2063777977 (DE-He213)04yd0085-p |
| title_full |
Cataclastic rheology of carbonate rocks |
| author_sort |
Lu, Xiancai |
| journal |
Science in China / D |
| journalStr |
Science in China / D |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
500 - Science |
| recordtype |
marc |
| publishDateSort |
2005 |
| contenttype_str_mv |
txt |
| container_start_page |
1227 |
| author_browse |
Lu, Xiancai Sun, Yan Shu, Liangshu Gu, Lianxing Guo, Jichun Zhu, Wenbin |
| container_volume |
48 |
| class |
550 VZ 13 ssgn |
| format_se |
Aufsätze |
| author-letter |
Lu, Xiancai |
| doi_str_mv |
10.1360/04yd0085 |
| dewey-full |
550 |
| title_sort |
cataclastic rheology of carbonate rocks |
| title_auth |
Cataclastic rheology of carbonate rocks |
| abstract |
Abstract Based on the knowledge of the shallow-level mylonitization of detrital rocks and intrusive rocks, the poorly-known cataclastic rheology of carbonate rocks is discussed comprehensively in this paper. The cases taken from eastern China are analyzed in various aspects including ductile-brittle fault zone, rock texture and structure, clastomylonite layer, leucocratic stress minerals, and frictional dynamometamorphism. It is proposed that the cataclastic flow structure represented by clastomylonite texture is a cooling pattern of flow assemblage characterized by cooling metamorphism, cooling mylonite and cooling stress minerals. Such a pattern is formed generally in mildly reducing physicochemical environments, and is commonly related to regional tectonism and mesothermal and epithermal mineralization. © Science in China Press 2005 |
| abstractGer |
Abstract Based on the knowledge of the shallow-level mylonitization of detrital rocks and intrusive rocks, the poorly-known cataclastic rheology of carbonate rocks is discussed comprehensively in this paper. The cases taken from eastern China are analyzed in various aspects including ductile-brittle fault zone, rock texture and structure, clastomylonite layer, leucocratic stress minerals, and frictional dynamometamorphism. It is proposed that the cataclastic flow structure represented by clastomylonite texture is a cooling pattern of flow assemblage characterized by cooling metamorphism, cooling mylonite and cooling stress minerals. Such a pattern is formed generally in mildly reducing physicochemical environments, and is commonly related to regional tectonism and mesothermal and epithermal mineralization. © Science in China Press 2005 |
| abstract_unstemmed |
Abstract Based on the knowledge of the shallow-level mylonitization of detrital rocks and intrusive rocks, the poorly-known cataclastic rheology of carbonate rocks is discussed comprehensively in this paper. The cases taken from eastern China are analyzed in various aspects including ductile-brittle fault zone, rock texture and structure, clastomylonite layer, leucocratic stress minerals, and frictional dynamometamorphism. It is proposed that the cataclastic flow structure represented by clastomylonite texture is a cooling pattern of flow assemblage characterized by cooling metamorphism, cooling mylonite and cooling stress minerals. Such a pattern is formed generally in mildly reducing physicochemical environments, and is commonly related to regional tectonism and mesothermal and epithermal mineralization. © Science in China Press 2005 |
| collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_4082 |
| container_issue |
8 |
| title_short |
Cataclastic rheology of carbonate rocks |
| url |
https://doi.org/10.1360/04yd0085 |
| remote_bool |
false |
| author2 |
Sun, Yan Shu, Liangshu Gu, Lianxing Guo, Jichun Zhu, Wenbin |
| author2Str |
Sun, Yan Shu, Liangshu Gu, Lianxing Guo, Jichun Zhu, Wenbin |
| ppnlink |
193118238 |
| mediatype_str_mv |
n |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| doi_str |
10.1360/04yd0085 |
| up_date |
2024-07-03T20:14:34.594Z |
| _version_ |
1803590224682418176 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2063777977</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230504094349.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200820s2005 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1360/04yd0085</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2063777977</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)04yd0085-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Lu, Xiancai</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Cataclastic rheology of carbonate rocks</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2005</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Science in China Press 2005</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Based on the knowledge of the shallow-level mylonitization of detrital rocks and intrusive rocks, the poorly-known cataclastic rheology of carbonate rocks is discussed comprehensively in this paper. The cases taken from eastern China are analyzed in various aspects including ductile-brittle fault zone, rock texture and structure, clastomylonite layer, leucocratic stress minerals, and frictional dynamometamorphism. It is proposed that the cataclastic flow structure represented by clastomylonite texture is a cooling pattern of flow assemblage characterized by cooling metamorphism, cooling mylonite and cooling stress minerals. Such a pattern is formed generally in mildly reducing physicochemical environments, and is commonly related to regional tectonism and mesothermal and epithermal mineralization.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">carbonate rock</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">cataclastic rheology</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">clastomylonite</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">ductile-brittle fault zone</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Sun, Yan</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Shu, Liangshu</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Gu, Lianxing</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Guo, Jichun</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhu, Wenbin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Science in China / D</subfield><subfield code="d">Science in China Press, 1996</subfield><subfield code="g">48(2005), 8 vom: Aug., Seite 1227-1233</subfield><subfield code="w">(DE-627)193118238</subfield><subfield code="w">(DE-600)1307899-9</subfield><subfield code="w">(DE-576)062316923</subfield><subfield code="x">1006-9313</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:48</subfield><subfield code="g">year:2005</subfield><subfield code="g">number:8</subfield><subfield code="g">month:08</subfield><subfield code="g">pages:1227-1233</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1360/04yd0085</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-OAS</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-MFO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4082</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">48</subfield><subfield code="j">2005</subfield><subfield code="e">8</subfield><subfield code="c">08</subfield><subfield code="h">1227-1233</subfield></datafield></record></collection>
|
| score |
7.401043 |