Dragons, brimstone and the geology of a volcanic arc on the island of the last Samurai, Kyushu, Japan
Not even Hollywood could dream of a place so magical as Kyushu. The southern‐most of the four major islands of the Japanese archipelago, this is a land of volcanoes, dinosaurs, and the last stand of the Samurai. And for good measure, James Bond visited here too, in the 1967 film You Only Live Twice...
Ausführliche Beschreibung
Autor*in: |
Williams, Mark [verfasserIn] |
---|
Format: |
Artikel |
---|---|
Sprache: |
Englisch |
Erschienen: |
2016 |
---|
Rechteinformationen: |
Nutzungsrecht: © 2016 John Wiley & Sons Ltd, The Geologists' Association & The Geological Society of London |
---|
Schlagwörter: |
---|
Übergeordnetes Werk: |
Enthalten in: Geology today - Oxford : Blackwell, 1985, 32(2016), 1, Seite 21-26 |
---|---|
Übergeordnetes Werk: |
volume:32 ; year:2016 ; number:1 ; pages:21-26 |
Links: |
---|
DOI / URN: |
10.1111/gto.12124 |
---|
Katalog-ID: |
OLC1971148350 |
---|
LEADER | 01000caa a2200265 4500 | ||
---|---|---|---|
001 | OLC1971148350 | ||
003 | DE-627 | ||
005 | 20220217061028.0 | ||
007 | tu | ||
008 | 160212s2016 xx ||||| 00| ||eng c | ||
024 | 7 | |a 10.1111/gto.12124 |2 doi | |
028 | 5 | 2 | |a PQ20160430 |
035 | |a (DE-627)OLC1971148350 | ||
035 | |a (DE-599)GBVOLC1971148350 | ||
035 | |a (PRQ)p684-fec8212fd440780dee0b83c4c5f023afc4a37ef6b0ff6984154824ff83b10d220 | ||
035 | |a (KEY)0172623420160000032000100021dragonsbrimstoneandthegeologyofavolcanicarcontheis | ||
040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
041 | |a eng | ||
082 | 0 | 4 | |a 550 |q ZDB |
084 | |a 38.10 |2 bkl | ||
100 | 1 | |a Williams, Mark |e verfasserin |4 aut | |
245 | 1 | 0 | |a Dragons, brimstone and the geology of a volcanic arc on the island of the last Samurai, Kyushu, Japan |
264 | 1 | |c 2016 | |
336 | |a Text |b txt |2 rdacontent | ||
337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
338 | |a Band |b nc |2 rdacarrier | ||
520 | |a Not even Hollywood could dream of a place so magical as Kyushu. The southern‐most of the four major islands of the Japanese archipelago, this is a land of volcanoes, dinosaurs, and the last stand of the Samurai. And for good measure, James Bond visited here too, in the 1967 film You Only Live Twice . The final explosive scenes of that film featured the destruction of megalomaniac Ernst Stavro Blofeld's headquarters hidden inside the crater of one of Kyushu's most emblematic volcanoes, Shinmoedake. Kyushu also straddles the largest geological structure in Japan, the Median Tectonic Line (MTL) that runs from the western approaches of the island to the central part of Honshu. The MTL has been active since the Cretaceous, and the sedimentary basins formed along its line in Kyushu contain some of Japan's most famous dinosaur finds. The MTL also defines a fundamental divide between the geological histories of the terranes north and south of its line, a history that takes us back to the origins of the Japanese archipelago half a billion years ago. | ||
540 | |a Nutzungsrecht: © 2016 John Wiley & Sons Ltd, The Geologists' Association & The Geological Society of London | ||
650 | 4 | |a Plate tectonics | |
650 | 4 | |a Evolution | |
650 | 4 | |a Volcanology | |
700 | 1 | |a Wallis, Simon |4 oth | |
700 | 1 | |a Komatsu, Toshifumi |4 oth | |
700 | 1 | |a Tanaka, Gengo |4 oth | |
700 | 1 | |a Oji, Tatsuo |4 oth | |
700 | 1 | |a Clark, Nicola |4 oth | |
773 | 0 | 8 | |i Enthalten in |t Geology today |d Oxford : Blackwell, 1985 |g 32(2016), 1, Seite 21-26 |w (DE-627)12916593X |w (DE-600)50456-7 |w (DE-576)034178163 |x 0266-6979 |7 nnns |
773 | 1 | 8 | |g volume:32 |g year:2016 |g number:1 |g pages:21-26 |
856 | 4 | 1 | |u http://dx.doi.org/10.1111/gto.12124 |3 Volltext |
856 | 4 | 2 | |u http://onlinelibrary.wiley.com/doi/10.1111/gto.12124/abstract |
856 | 4 | 2 | |u http://search.proquest.com/docview/1760264669 |
912 | |a GBV_USEFLAG_A | ||
912 | |a SYSFLAG_A | ||
912 | |a GBV_OLC | ||
912 | |a SSG-OLC-GEO | ||
912 | |a SSG-OPC-GGO | ||
936 | b | k | |a 38.10 |q AVZ |
951 | |a AR | ||
952 | |d 32 |j 2016 |e 1 |h 21-26 |
author_variant |
m w mw |
---|---|
matchkey_str |
article:02666979:2016----::rgnbisoenteelgoaocncrotesadfhl |
hierarchy_sort_str |
2016 |
bklnumber |
38.10 |
publishDate |
2016 |
allfields |
10.1111/gto.12124 doi PQ20160430 (DE-627)OLC1971148350 (DE-599)GBVOLC1971148350 (PRQ)p684-fec8212fd440780dee0b83c4c5f023afc4a37ef6b0ff6984154824ff83b10d220 (KEY)0172623420160000032000100021dragonsbrimstoneandthegeologyofavolcanicarcontheis DE-627 ger DE-627 rakwb eng 550 ZDB 38.10 bkl Williams, Mark verfasserin aut Dragons, brimstone and the geology of a volcanic arc on the island of the last Samurai, Kyushu, Japan 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Not even Hollywood could dream of a place so magical as Kyushu. The southern‐most of the four major islands of the Japanese archipelago, this is a land of volcanoes, dinosaurs, and the last stand of the Samurai. And for good measure, James Bond visited here too, in the 1967 film You Only Live Twice . The final explosive scenes of that film featured the destruction of megalomaniac Ernst Stavro Blofeld's headquarters hidden inside the crater of one of Kyushu's most emblematic volcanoes, Shinmoedake. Kyushu also straddles the largest geological structure in Japan, the Median Tectonic Line (MTL) that runs from the western approaches of the island to the central part of Honshu. The MTL has been active since the Cretaceous, and the sedimentary basins formed along its line in Kyushu contain some of Japan's most famous dinosaur finds. The MTL also defines a fundamental divide between the geological histories of the terranes north and south of its line, a history that takes us back to the origins of the Japanese archipelago half a billion years ago. Nutzungsrecht: © 2016 John Wiley & Sons Ltd, The Geologists' Association & The Geological Society of London Plate tectonics Evolution Volcanology Wallis, Simon oth Komatsu, Toshifumi oth Tanaka, Gengo oth Oji, Tatsuo oth Clark, Nicola oth Enthalten in Geology today Oxford : Blackwell, 1985 32(2016), 1, Seite 21-26 (DE-627)12916593X (DE-600)50456-7 (DE-576)034178163 0266-6979 nnns volume:32 year:2016 number:1 pages:21-26 http://dx.doi.org/10.1111/gto.12124 Volltext http://onlinelibrary.wiley.com/doi/10.1111/gto.12124/abstract http://search.proquest.com/docview/1760264669 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO 38.10 AVZ AR 32 2016 1 21-26 |
spelling |
10.1111/gto.12124 doi PQ20160430 (DE-627)OLC1971148350 (DE-599)GBVOLC1971148350 (PRQ)p684-fec8212fd440780dee0b83c4c5f023afc4a37ef6b0ff6984154824ff83b10d220 (KEY)0172623420160000032000100021dragonsbrimstoneandthegeologyofavolcanicarcontheis DE-627 ger DE-627 rakwb eng 550 ZDB 38.10 bkl Williams, Mark verfasserin aut Dragons, brimstone and the geology of a volcanic arc on the island of the last Samurai, Kyushu, Japan 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Not even Hollywood could dream of a place so magical as Kyushu. The southern‐most of the four major islands of the Japanese archipelago, this is a land of volcanoes, dinosaurs, and the last stand of the Samurai. And for good measure, James Bond visited here too, in the 1967 film You Only Live Twice . The final explosive scenes of that film featured the destruction of megalomaniac Ernst Stavro Blofeld's headquarters hidden inside the crater of one of Kyushu's most emblematic volcanoes, Shinmoedake. Kyushu also straddles the largest geological structure in Japan, the Median Tectonic Line (MTL) that runs from the western approaches of the island to the central part of Honshu. The MTL has been active since the Cretaceous, and the sedimentary basins formed along its line in Kyushu contain some of Japan's most famous dinosaur finds. The MTL also defines a fundamental divide between the geological histories of the terranes north and south of its line, a history that takes us back to the origins of the Japanese archipelago half a billion years ago. Nutzungsrecht: © 2016 John Wiley & Sons Ltd, The Geologists' Association & The Geological Society of London Plate tectonics Evolution Volcanology Wallis, Simon oth Komatsu, Toshifumi oth Tanaka, Gengo oth Oji, Tatsuo oth Clark, Nicola oth Enthalten in Geology today Oxford : Blackwell, 1985 32(2016), 1, Seite 21-26 (DE-627)12916593X (DE-600)50456-7 (DE-576)034178163 0266-6979 nnns volume:32 year:2016 number:1 pages:21-26 http://dx.doi.org/10.1111/gto.12124 Volltext http://onlinelibrary.wiley.com/doi/10.1111/gto.12124/abstract http://search.proquest.com/docview/1760264669 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO 38.10 AVZ AR 32 2016 1 21-26 |
allfields_unstemmed |
10.1111/gto.12124 doi PQ20160430 (DE-627)OLC1971148350 (DE-599)GBVOLC1971148350 (PRQ)p684-fec8212fd440780dee0b83c4c5f023afc4a37ef6b0ff6984154824ff83b10d220 (KEY)0172623420160000032000100021dragonsbrimstoneandthegeologyofavolcanicarcontheis DE-627 ger DE-627 rakwb eng 550 ZDB 38.10 bkl Williams, Mark verfasserin aut Dragons, brimstone and the geology of a volcanic arc on the island of the last Samurai, Kyushu, Japan 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Not even Hollywood could dream of a place so magical as Kyushu. The southern‐most of the four major islands of the Japanese archipelago, this is a land of volcanoes, dinosaurs, and the last stand of the Samurai. And for good measure, James Bond visited here too, in the 1967 film You Only Live Twice . The final explosive scenes of that film featured the destruction of megalomaniac Ernst Stavro Blofeld's headquarters hidden inside the crater of one of Kyushu's most emblematic volcanoes, Shinmoedake. Kyushu also straddles the largest geological structure in Japan, the Median Tectonic Line (MTL) that runs from the western approaches of the island to the central part of Honshu. The MTL has been active since the Cretaceous, and the sedimentary basins formed along its line in Kyushu contain some of Japan's most famous dinosaur finds. The MTL also defines a fundamental divide between the geological histories of the terranes north and south of its line, a history that takes us back to the origins of the Japanese archipelago half a billion years ago. Nutzungsrecht: © 2016 John Wiley & Sons Ltd, The Geologists' Association & The Geological Society of London Plate tectonics Evolution Volcanology Wallis, Simon oth Komatsu, Toshifumi oth Tanaka, Gengo oth Oji, Tatsuo oth Clark, Nicola oth Enthalten in Geology today Oxford : Blackwell, 1985 32(2016), 1, Seite 21-26 (DE-627)12916593X (DE-600)50456-7 (DE-576)034178163 0266-6979 nnns volume:32 year:2016 number:1 pages:21-26 http://dx.doi.org/10.1111/gto.12124 Volltext http://onlinelibrary.wiley.com/doi/10.1111/gto.12124/abstract http://search.proquest.com/docview/1760264669 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO 38.10 AVZ AR 32 2016 1 21-26 |
allfieldsGer |
10.1111/gto.12124 doi PQ20160430 (DE-627)OLC1971148350 (DE-599)GBVOLC1971148350 (PRQ)p684-fec8212fd440780dee0b83c4c5f023afc4a37ef6b0ff6984154824ff83b10d220 (KEY)0172623420160000032000100021dragonsbrimstoneandthegeologyofavolcanicarcontheis DE-627 ger DE-627 rakwb eng 550 ZDB 38.10 bkl Williams, Mark verfasserin aut Dragons, brimstone and the geology of a volcanic arc on the island of the last Samurai, Kyushu, Japan 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Not even Hollywood could dream of a place so magical as Kyushu. The southern‐most of the four major islands of the Japanese archipelago, this is a land of volcanoes, dinosaurs, and the last stand of the Samurai. And for good measure, James Bond visited here too, in the 1967 film You Only Live Twice . The final explosive scenes of that film featured the destruction of megalomaniac Ernst Stavro Blofeld's headquarters hidden inside the crater of one of Kyushu's most emblematic volcanoes, Shinmoedake. Kyushu also straddles the largest geological structure in Japan, the Median Tectonic Line (MTL) that runs from the western approaches of the island to the central part of Honshu. The MTL has been active since the Cretaceous, and the sedimentary basins formed along its line in Kyushu contain some of Japan's most famous dinosaur finds. The MTL also defines a fundamental divide between the geological histories of the terranes north and south of its line, a history that takes us back to the origins of the Japanese archipelago half a billion years ago. Nutzungsrecht: © 2016 John Wiley & Sons Ltd, The Geologists' Association & The Geological Society of London Plate tectonics Evolution Volcanology Wallis, Simon oth Komatsu, Toshifumi oth Tanaka, Gengo oth Oji, Tatsuo oth Clark, Nicola oth Enthalten in Geology today Oxford : Blackwell, 1985 32(2016), 1, Seite 21-26 (DE-627)12916593X (DE-600)50456-7 (DE-576)034178163 0266-6979 nnns volume:32 year:2016 number:1 pages:21-26 http://dx.doi.org/10.1111/gto.12124 Volltext http://onlinelibrary.wiley.com/doi/10.1111/gto.12124/abstract http://search.proquest.com/docview/1760264669 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO 38.10 AVZ AR 32 2016 1 21-26 |
allfieldsSound |
10.1111/gto.12124 doi PQ20160430 (DE-627)OLC1971148350 (DE-599)GBVOLC1971148350 (PRQ)p684-fec8212fd440780dee0b83c4c5f023afc4a37ef6b0ff6984154824ff83b10d220 (KEY)0172623420160000032000100021dragonsbrimstoneandthegeologyofavolcanicarcontheis DE-627 ger DE-627 rakwb eng 550 ZDB 38.10 bkl Williams, Mark verfasserin aut Dragons, brimstone and the geology of a volcanic arc on the island of the last Samurai, Kyushu, Japan 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Not even Hollywood could dream of a place so magical as Kyushu. The southern‐most of the four major islands of the Japanese archipelago, this is a land of volcanoes, dinosaurs, and the last stand of the Samurai. And for good measure, James Bond visited here too, in the 1967 film You Only Live Twice . The final explosive scenes of that film featured the destruction of megalomaniac Ernst Stavro Blofeld's headquarters hidden inside the crater of one of Kyushu's most emblematic volcanoes, Shinmoedake. Kyushu also straddles the largest geological structure in Japan, the Median Tectonic Line (MTL) that runs from the western approaches of the island to the central part of Honshu. The MTL has been active since the Cretaceous, and the sedimentary basins formed along its line in Kyushu contain some of Japan's most famous dinosaur finds. The MTL also defines a fundamental divide between the geological histories of the terranes north and south of its line, a history that takes us back to the origins of the Japanese archipelago half a billion years ago. Nutzungsrecht: © 2016 John Wiley & Sons Ltd, The Geologists' Association & The Geological Society of London Plate tectonics Evolution Volcanology Wallis, Simon oth Komatsu, Toshifumi oth Tanaka, Gengo oth Oji, Tatsuo oth Clark, Nicola oth Enthalten in Geology today Oxford : Blackwell, 1985 32(2016), 1, Seite 21-26 (DE-627)12916593X (DE-600)50456-7 (DE-576)034178163 0266-6979 nnns volume:32 year:2016 number:1 pages:21-26 http://dx.doi.org/10.1111/gto.12124 Volltext http://onlinelibrary.wiley.com/doi/10.1111/gto.12124/abstract http://search.proquest.com/docview/1760264669 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO 38.10 AVZ AR 32 2016 1 21-26 |
language |
English |
source |
Enthalten in Geology today 32(2016), 1, Seite 21-26 volume:32 year:2016 number:1 pages:21-26 |
sourceStr |
Enthalten in Geology today 32(2016), 1, Seite 21-26 volume:32 year:2016 number:1 pages:21-26 |
format_phy_str_mv |
Article |
institution |
findex.gbv.de |
topic_facet |
Plate tectonics Evolution Volcanology |
dewey-raw |
550 |
isfreeaccess_bool |
false |
container_title |
Geology today |
authorswithroles_txt_mv |
Williams, Mark @@aut@@ Wallis, Simon @@oth@@ Komatsu, Toshifumi @@oth@@ Tanaka, Gengo @@oth@@ Oji, Tatsuo @@oth@@ Clark, Nicola @@oth@@ |
publishDateDaySort_date |
2016-01-01T00:00:00Z |
hierarchy_top_id |
12916593X |
dewey-sort |
3550 |
id |
OLC1971148350 |
language_de |
englisch |
fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a2200265 4500</leader><controlfield tag="001">OLC1971148350</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220217061028.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">160212s2016 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1111/gto.12124</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">PQ20160430</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC1971148350</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)GBVOLC1971148350</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(PRQ)p684-fec8212fd440780dee0b83c4c5f023afc4a37ef6b0ff6984154824ff83b10d220</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(KEY)0172623420160000032000100021dragonsbrimstoneandthegeologyofavolcanicarcontheis</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">ZDB</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.10</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Williams, Mark</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Dragons, brimstone and the geology of a volcanic arc on the island of the last Samurai, Kyushu, Japan</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2016</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="520" ind1=" " ind2=" "><subfield code="a">Not even Hollywood could dream of a place so magical as Kyushu. The southern‐most of the four major islands of the Japanese archipelago, this is a land of volcanoes, dinosaurs, and the last stand of the Samurai. And for good measure, James Bond visited here too, in the 1967 film You Only Live Twice . The final explosive scenes of that film featured the destruction of megalomaniac Ernst Stavro Blofeld's headquarters hidden inside the crater of one of Kyushu's most emblematic volcanoes, Shinmoedake. Kyushu also straddles the largest geological structure in Japan, the Median Tectonic Line (MTL) that runs from the western approaches of the island to the central part of Honshu. The MTL has been active since the Cretaceous, and the sedimentary basins formed along its line in Kyushu contain some of Japan's most famous dinosaur finds. The MTL also defines a fundamental divide between the geological histories of the terranes north and south of its line, a history that takes us back to the origins of the Japanese archipelago half a billion years ago.</subfield></datafield><datafield tag="540" ind1=" " ind2=" "><subfield code="a">Nutzungsrecht: © 2016 John Wiley & Sons Ltd, The Geologists' Association & The Geological Society of London</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Plate tectonics</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Evolution</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Volcanology</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wallis, Simon</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Komatsu, Toshifumi</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Tanaka, Gengo</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Oji, Tatsuo</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Clark, Nicola</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Geology today</subfield><subfield code="d">Oxford : Blackwell, 1985</subfield><subfield code="g">32(2016), 1, Seite 21-26</subfield><subfield code="w">(DE-627)12916593X</subfield><subfield code="w">(DE-600)50456-7</subfield><subfield code="w">(DE-576)034178163</subfield><subfield code="x">0266-6979</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:32</subfield><subfield code="g">year:2016</subfield><subfield code="g">number:1</subfield><subfield code="g">pages:21-26</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">http://dx.doi.org/10.1111/gto.12124</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://onlinelibrary.wiley.com/doi/10.1111/gto.12124/abstract</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://search.proquest.com/docview/1760264669</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-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">38.10</subfield><subfield code="q">AVZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">32</subfield><subfield code="j">2016</subfield><subfield code="e">1</subfield><subfield code="h">21-26</subfield></datafield></record></collection>
|
author |
Williams, Mark |
spellingShingle |
Williams, Mark ddc 550 bkl 38.10 misc Plate tectonics misc Evolution misc Volcanology Dragons, brimstone and the geology of a volcanic arc on the island of the last Samurai, Kyushu, Japan |
authorStr |
Williams, Mark |
ppnlink_with_tag_str_mv |
@@773@@(DE-627)12916593X |
format |
Article |
dewey-ones |
550 - Earth sciences |
delete_txt_mv |
keep |
author_role |
aut |
collection |
OLC |
remote_str |
false |
illustrated |
Not Illustrated |
issn |
0266-6979 |
topic_title |
550 ZDB 38.10 bkl Dragons, brimstone and the geology of a volcanic arc on the island of the last Samurai, Kyushu, Japan Plate tectonics Evolution Volcanology |
topic |
ddc 550 bkl 38.10 misc Plate tectonics misc Evolution misc Volcanology |
topic_unstemmed |
ddc 550 bkl 38.10 misc Plate tectonics misc Evolution misc Volcanology |
topic_browse |
ddc 550 bkl 38.10 misc Plate tectonics misc Evolution misc Volcanology |
format_facet |
Aufsätze Gedruckte Aufsätze |
format_main_str_mv |
Text Zeitschrift/Artikel |
carriertype_str_mv |
nc |
author2_variant |
s w sw t k tk g t gt t o to n c nc |
hierarchy_parent_title |
Geology today |
hierarchy_parent_id |
12916593X |
dewey-tens |
550 - Earth sciences & geology |
hierarchy_top_title |
Geology today |
isfreeaccess_txt |
false |
familylinks_str_mv |
(DE-627)12916593X (DE-600)50456-7 (DE-576)034178163 |
title |
Dragons, brimstone and the geology of a volcanic arc on the island of the last Samurai, Kyushu, Japan |
ctrlnum |
(DE-627)OLC1971148350 (DE-599)GBVOLC1971148350 (PRQ)p684-fec8212fd440780dee0b83c4c5f023afc4a37ef6b0ff6984154824ff83b10d220 (KEY)0172623420160000032000100021dragonsbrimstoneandthegeologyofavolcanicarcontheis |
title_full |
Dragons, brimstone and the geology of a volcanic arc on the island of the last Samurai, Kyushu, Japan |
author_sort |
Williams, Mark |
journal |
Geology today |
journalStr |
Geology today |
lang_code |
eng |
isOA_bool |
false |
dewey-hundreds |
500 - Science |
recordtype |
marc |
publishDateSort |
2016 |
contenttype_str_mv |
txt |
container_start_page |
21 |
author_browse |
Williams, Mark |
container_volume |
32 |
class |
550 ZDB 38.10 bkl |
format_se |
Aufsätze |
author-letter |
Williams, Mark |
doi_str_mv |
10.1111/gto.12124 |
dewey-full |
550 |
title_sort |
dragons, brimstone and the geology of a volcanic arc on the island of the last samurai, kyushu, japan |
title_auth |
Dragons, brimstone and the geology of a volcanic arc on the island of the last Samurai, Kyushu, Japan |
abstract |
Not even Hollywood could dream of a place so magical as Kyushu. The southern‐most of the four major islands of the Japanese archipelago, this is a land of volcanoes, dinosaurs, and the last stand of the Samurai. And for good measure, James Bond visited here too, in the 1967 film You Only Live Twice . The final explosive scenes of that film featured the destruction of megalomaniac Ernst Stavro Blofeld's headquarters hidden inside the crater of one of Kyushu's most emblematic volcanoes, Shinmoedake. Kyushu also straddles the largest geological structure in Japan, the Median Tectonic Line (MTL) that runs from the western approaches of the island to the central part of Honshu. The MTL has been active since the Cretaceous, and the sedimentary basins formed along its line in Kyushu contain some of Japan's most famous dinosaur finds. The MTL also defines a fundamental divide between the geological histories of the terranes north and south of its line, a history that takes us back to the origins of the Japanese archipelago half a billion years ago. |
abstractGer |
Not even Hollywood could dream of a place so magical as Kyushu. The southern‐most of the four major islands of the Japanese archipelago, this is a land of volcanoes, dinosaurs, and the last stand of the Samurai. And for good measure, James Bond visited here too, in the 1967 film You Only Live Twice . The final explosive scenes of that film featured the destruction of megalomaniac Ernst Stavro Blofeld's headquarters hidden inside the crater of one of Kyushu's most emblematic volcanoes, Shinmoedake. Kyushu also straddles the largest geological structure in Japan, the Median Tectonic Line (MTL) that runs from the western approaches of the island to the central part of Honshu. The MTL has been active since the Cretaceous, and the sedimentary basins formed along its line in Kyushu contain some of Japan's most famous dinosaur finds. The MTL also defines a fundamental divide between the geological histories of the terranes north and south of its line, a history that takes us back to the origins of the Japanese archipelago half a billion years ago. |
abstract_unstemmed |
Not even Hollywood could dream of a place so magical as Kyushu. The southern‐most of the four major islands of the Japanese archipelago, this is a land of volcanoes, dinosaurs, and the last stand of the Samurai. And for good measure, James Bond visited here too, in the 1967 film You Only Live Twice . The final explosive scenes of that film featured the destruction of megalomaniac Ernst Stavro Blofeld's headquarters hidden inside the crater of one of Kyushu's most emblematic volcanoes, Shinmoedake. Kyushu also straddles the largest geological structure in Japan, the Median Tectonic Line (MTL) that runs from the western approaches of the island to the central part of Honshu. The MTL has been active since the Cretaceous, and the sedimentary basins formed along its line in Kyushu contain some of Japan's most famous dinosaur finds. The MTL also defines a fundamental divide between the geological histories of the terranes north and south of its line, a history that takes us back to the origins of the Japanese archipelago half a billion years ago. |
collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO |
container_issue |
1 |
title_short |
Dragons, brimstone and the geology of a volcanic arc on the island of the last Samurai, Kyushu, Japan |
url |
http://dx.doi.org/10.1111/gto.12124 http://onlinelibrary.wiley.com/doi/10.1111/gto.12124/abstract http://search.proquest.com/docview/1760264669 |
remote_bool |
false |
author2 |
Wallis, Simon Komatsu, Toshifumi Tanaka, Gengo Oji, Tatsuo Clark, Nicola |
author2Str |
Wallis, Simon Komatsu, Toshifumi Tanaka, Gengo Oji, Tatsuo Clark, Nicola |
ppnlink |
12916593X |
mediatype_str_mv |
n |
isOA_txt |
false |
hochschulschrift_bool |
false |
author2_role |
oth oth oth oth oth |
doi_str |
10.1111/gto.12124 |
up_date |
2024-07-03T18:22:45.985Z |
_version_ |
1803583190189735936 |
fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a2200265 4500</leader><controlfield tag="001">OLC1971148350</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220217061028.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">160212s2016 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1111/gto.12124</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">PQ20160430</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC1971148350</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)GBVOLC1971148350</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(PRQ)p684-fec8212fd440780dee0b83c4c5f023afc4a37ef6b0ff6984154824ff83b10d220</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(KEY)0172623420160000032000100021dragonsbrimstoneandthegeologyofavolcanicarcontheis</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">ZDB</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.10</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Williams, Mark</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Dragons, brimstone and the geology of a volcanic arc on the island of the last Samurai, Kyushu, Japan</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2016</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="520" ind1=" " ind2=" "><subfield code="a">Not even Hollywood could dream of a place so magical as Kyushu. The southern‐most of the four major islands of the Japanese archipelago, this is a land of volcanoes, dinosaurs, and the last stand of the Samurai. And for good measure, James Bond visited here too, in the 1967 film You Only Live Twice . The final explosive scenes of that film featured the destruction of megalomaniac Ernst Stavro Blofeld's headquarters hidden inside the crater of one of Kyushu's most emblematic volcanoes, Shinmoedake. Kyushu also straddles the largest geological structure in Japan, the Median Tectonic Line (MTL) that runs from the western approaches of the island to the central part of Honshu. The MTL has been active since the Cretaceous, and the sedimentary basins formed along its line in Kyushu contain some of Japan's most famous dinosaur finds. The MTL also defines a fundamental divide between the geological histories of the terranes north and south of its line, a history that takes us back to the origins of the Japanese archipelago half a billion years ago.</subfield></datafield><datafield tag="540" ind1=" " ind2=" "><subfield code="a">Nutzungsrecht: © 2016 John Wiley & Sons Ltd, The Geologists' Association & The Geological Society of London</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Plate tectonics</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Evolution</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Volcanology</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wallis, Simon</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Komatsu, Toshifumi</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Tanaka, Gengo</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Oji, Tatsuo</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Clark, Nicola</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Geology today</subfield><subfield code="d">Oxford : Blackwell, 1985</subfield><subfield code="g">32(2016), 1, Seite 21-26</subfield><subfield code="w">(DE-627)12916593X</subfield><subfield code="w">(DE-600)50456-7</subfield><subfield code="w">(DE-576)034178163</subfield><subfield code="x">0266-6979</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:32</subfield><subfield code="g">year:2016</subfield><subfield code="g">number:1</subfield><subfield code="g">pages:21-26</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">http://dx.doi.org/10.1111/gto.12124</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://onlinelibrary.wiley.com/doi/10.1111/gto.12124/abstract</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://search.proquest.com/docview/1760264669</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-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">38.10</subfield><subfield code="q">AVZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">32</subfield><subfield code="j">2016</subfield><subfield code="e">1</subfield><subfield code="h">21-26</subfield></datafield></record></collection>
|
score |
7.4005537 |