Research history of the Green Tuff region in NE Japan in relation to the Sea of Japan formation
Green Tuff comprising altered Neogene volcanic and volcaniclastic rocks occurs on the Sea of Japan side of Hokkaido, Fossa Magna, and Southwest Japan, and is widely distributed in Northeast Japan. This paper presents a review of the history of research on the geological development of the Green Tuff...
Gespeichert in:
| Veröffentlicht in: | Chishitsugaku zasshi 2021/07/15, Vol.127(7), pp.381-394 |
|---|---|
| Hauptverfasser: | , |
| Format: | Artikel |
| Sprache: | eng ; jpn |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 394 |
|---|---|
| container_issue | 7 |
| container_start_page | 381 |
| container_title | Chishitsugaku zasshi |
| container_volume | 127 |
| creator | Amano, Kazuo Hosoi, Jun |
| description | Green Tuff comprising altered Neogene volcanic and volcaniclastic rocks occurs on the Sea of Japan side of Hokkaido, Fossa Magna, and Southwest Japan, and is widely distributed in Northeast Japan. This paper presents a review of the history of research on the geological development of the Green Tuff in Northeast Japan in relation to the opening of the Sea of Japan. Research before 1970 was based mainly on the geosyncline paradigm; research after 1970, when the concept of plate tectonics was introduced, progressed in two stages. From early 1970 to about 2000, conventional stratigraphic data were summarized and tectonic models related to the opening of the Sea of Japan were presented. From about 2000 until now, new data have been provided by improved dating methods, paleomagnetic measurements, detailed restoration of paleoenvironments from sedimentary facies analysis, and restoration of stress fields, allowing the reconstruction of more advanced tectonic models. |
| doi_str_mv | 10.5575/geosoc.2020.0063 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2605287374</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2605287374</sourcerecordid><originalsourceid>FETCH-LOGICAL-a1993-9863a0dde6f2146246ef7b55f4562221941081e7842c7f0ae232221f0ab21ff73</originalsourceid><addsrcrecordid>eNo9kM1PAjEQxRujiQS5e2zieXHa7rbboyEIGqOJ4rkpy5RdAltslwP_vfuhXN5MZt5vJnmE3DOYZpnKHrfooy-mHDhMAaS4IiMmUp1oLcU1GQEwmSgp4JZMYqzWAKCFFIqPiPnEiDYUJS2r2Phwpt7RpkS6CIg1XZ2cowG3la9pVdP3OX21R9v3Afe26eaN74EvtB077J0Ph357R26c3Uec_NUx-X6er2bL5O1j8TJ7ekss01okOpfCwmaD0nGWSp5KdGqdZS7NJOec6ZRBzlDlKS-UA4tcdOO2W7fqlBiTh-HuMfifE8bG7Pwp1O1LwyVkPFdCpa0LBlcRfIwBnTmG6mDD2TAwXZJmSNJ0SZouyRZZDsguNnaLF8CGpir2-A8wrozq9YJeLEVpg8Fa_AJI-n8Y</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2605287374</pqid></control><display><type>article</type><title>Research history of the Green Tuff region in NE Japan in relation to the Sea of Japan formation</title><source>J-STAGE Free</source><source>Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals</source><creator>Amano, Kazuo ; Hosoi, Jun</creator><creatorcontrib>Amano, Kazuo ; Hosoi, Jun</creatorcontrib><description>Green Tuff comprising altered Neogene volcanic and volcaniclastic rocks occurs on the Sea of Japan side of Hokkaido, Fossa Magna, and Southwest Japan, and is widely distributed in Northeast Japan. This paper presents a review of the history of research on the geological development of the Green Tuff in Northeast Japan in relation to the opening of the Sea of Japan. Research before 1970 was based mainly on the geosyncline paradigm; research after 1970, when the concept of plate tectonics was introduced, progressed in two stages. From early 1970 to about 2000, conventional stratigraphic data were summarized and tectonic models related to the opening of the Sea of Japan were presented. From about 2000 until now, new data have been provided by improved dating methods, paleomagnetic measurements, detailed restoration of paleoenvironments from sedimentary facies analysis, and restoration of stress fields, allowing the reconstruction of more advanced tectonic models.</description><identifier>ISSN: 0016-7630</identifier><identifier>EISSN: 1349-9963</identifier><identifier>DOI: 10.5575/geosoc.2020.0063</identifier><language>eng ; jpn</language><publisher>Tokyo: The Geological Society of Japan</publisher><subject>Fossils ; Geosynclines ; Green Tuff ; Miocene ; Neogene ; Northeast Japan ; Palaeomagnetism ; Paleomagnetism ; Plate tectonics ; Restoration ; Sea of Japan opening ; Sedimentary facies ; Tectonics</subject><ispartof>The Journal of the Geological Society of Japan, 2021/07/15, Vol.127(7), pp.381-394</ispartof><rights>2021 by The Geological Society of Japan</rights><rights>Copyright Japan Science and Technology Agency 2021</rights><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-a1993-9863a0dde6f2146246ef7b55f4562221941081e7842c7f0ae232221f0ab21ff73</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,1876,27903,27904</link.rule.ids></links><search><creatorcontrib>Amano, Kazuo</creatorcontrib><creatorcontrib>Hosoi, Jun</creatorcontrib><title>Research history of the Green Tuff region in NE Japan in relation to the Sea of Japan formation</title><title>Chishitsugaku zasshi</title><addtitle>Jour. Geol. Soc. Japan</addtitle><description>Green Tuff comprising altered Neogene volcanic and volcaniclastic rocks occurs on the Sea of Japan side of Hokkaido, Fossa Magna, and Southwest Japan, and is widely distributed in Northeast Japan. This paper presents a review of the history of research on the geological development of the Green Tuff in Northeast Japan in relation to the opening of the Sea of Japan. Research before 1970 was based mainly on the geosyncline paradigm; research after 1970, when the concept of plate tectonics was introduced, progressed in two stages. From early 1970 to about 2000, conventional stratigraphic data were summarized and tectonic models related to the opening of the Sea of Japan were presented. From about 2000 until now, new data have been provided by improved dating methods, paleomagnetic measurements, detailed restoration of paleoenvironments from sedimentary facies analysis, and restoration of stress fields, allowing the reconstruction of more advanced tectonic models.</description><subject>Fossils</subject><subject>Geosynclines</subject><subject>Green Tuff</subject><subject>Miocene</subject><subject>Neogene</subject><subject>Northeast Japan</subject><subject>Palaeomagnetism</subject><subject>Paleomagnetism</subject><subject>Plate tectonics</subject><subject>Restoration</subject><subject>Sea of Japan opening</subject><subject>Sedimentary facies</subject><subject>Tectonics</subject><issn>0016-7630</issn><issn>1349-9963</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNo9kM1PAjEQxRujiQS5e2zieXHa7rbboyEIGqOJ4rkpy5RdAltslwP_vfuhXN5MZt5vJnmE3DOYZpnKHrfooy-mHDhMAaS4IiMmUp1oLcU1GQEwmSgp4JZMYqzWAKCFFIqPiPnEiDYUJS2r2Phwpt7RpkS6CIg1XZ2cowG3la9pVdP3OX21R9v3Afe26eaN74EvtB077J0Ph357R26c3Uec_NUx-X6er2bL5O1j8TJ7ekss01okOpfCwmaD0nGWSp5KdGqdZS7NJOec6ZRBzlDlKS-UA4tcdOO2W7fqlBiTh-HuMfifE8bG7Pwp1O1LwyVkPFdCpa0LBlcRfIwBnTmG6mDD2TAwXZJmSNJ0SZouyRZZDsguNnaLF8CGpir2-A8wrozq9YJeLEVpg8Fa_AJI-n8Y</recordid><startdate>20210715</startdate><enddate>20210715</enddate><creator>Amano, Kazuo</creator><creator>Hosoi, Jun</creator><general>The Geological Society of Japan</general><general>Japan Science and Technology Agency</general><scope>AAYXX</scope><scope>CITATION</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>20210715</creationdate><title>Research history of the Green Tuff region in NE Japan in relation to the Sea of Japan formation</title><author>Amano, Kazuo ; Hosoi, Jun</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a1993-9863a0dde6f2146246ef7b55f4562221941081e7842c7f0ae232221f0ab21ff73</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng ; jpn</language><creationdate>2021</creationdate><topic>Fossils</topic><topic>Geosynclines</topic><topic>Green Tuff</topic><topic>Miocene</topic><topic>Neogene</topic><topic>Northeast Japan</topic><topic>Palaeomagnetism</topic><topic>Paleomagnetism</topic><topic>Plate tectonics</topic><topic>Restoration</topic><topic>Sea of Japan opening</topic><topic>Sedimentary facies</topic><topic>Tectonics</topic><toplevel>online_resources</toplevel><creatorcontrib>Amano, Kazuo</creatorcontrib><creatorcontrib>Hosoi, Jun</creatorcontrib><collection>CrossRef</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Chishitsugaku zasshi</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Amano, Kazuo</au><au>Hosoi, Jun</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Research history of the Green Tuff region in NE Japan in relation to the Sea of Japan formation</atitle><jtitle>Chishitsugaku zasshi</jtitle><addtitle>Jour. Geol. Soc. Japan</addtitle><date>2021-07-15</date><risdate>2021</risdate><volume>127</volume><issue>7</issue><spage>381</spage><epage>394</epage><pages>381-394</pages><artnum>2020.0063</artnum><issn>0016-7630</issn><eissn>1349-9963</eissn><abstract>Green Tuff comprising altered Neogene volcanic and volcaniclastic rocks occurs on the Sea of Japan side of Hokkaido, Fossa Magna, and Southwest Japan, and is widely distributed in Northeast Japan. This paper presents a review of the history of research on the geological development of the Green Tuff in Northeast Japan in relation to the opening of the Sea of Japan. Research before 1970 was based mainly on the geosyncline paradigm; research after 1970, when the concept of plate tectonics was introduced, progressed in two stages. From early 1970 to about 2000, conventional stratigraphic data were summarized and tectonic models related to the opening of the Sea of Japan were presented. From about 2000 until now, new data have been provided by improved dating methods, paleomagnetic measurements, detailed restoration of paleoenvironments from sedimentary facies analysis, and restoration of stress fields, allowing the reconstruction of more advanced tectonic models.</abstract><cop>Tokyo</cop><pub>The Geological Society of Japan</pub><doi>10.5575/geosoc.2020.0063</doi><tpages>14</tpages><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0016-7630 |
| ispartof | The Journal of the Geological Society of Japan, 2021/07/15, Vol.127(7), pp.381-394 |
| issn | 0016-7630 1349-9963 |
| language | eng ; jpn |
| recordid | cdi_proquest_journals_2605287374 |
| source | J-STAGE Free; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals |
| subjects | Fossils Geosynclines Green Tuff Miocene Neogene Northeast Japan Palaeomagnetism Paleomagnetism Plate tectonics Restoration Sea of Japan opening Sedimentary facies Tectonics |
| title | Research history of the Green Tuff region in NE Japan in relation to the Sea of Japan formation |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-21T20%3A06%3A03IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Research%20history%20of%20the%20Green%20Tuff%20region%20in%20NE%20Japan%20in%20relation%20to%20the%20Sea%20of%20Japan%20formation&rft.jtitle=Chishitsugaku%20zasshi&rft.au=Amano,%20Kazuo&rft.date=2021-07-15&rft.volume=127&rft.issue=7&rft.spage=381&rft.epage=394&rft.pages=381-394&rft.artnum=2020.0063&rft.issn=0016-7630&rft.eissn=1349-9963&rft_id=info:doi/10.5575/geosoc.2020.0063&rft_dat=%3Cproquest_cross%3E2605287374%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2605287374&rft_id=info:pmid/&rfr_iscdi=true |