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{{Short description|Oceanic Basin in the Sea of Japan}}
{{pp-semi-indef|small=yes}}
{{coord|36|34|48.89|N|131|38|57.01|E|scale:1000000|display=title}} {{coord|36|34|48.89|N|131|38|57.01|E|scale:1000000|display=title}}
{{Infobox East Asian {{Infobox transliteration
|title=Tsushima Basin<br />Ulleung Basin | title = Tsushima Basin<br />Ulleung Basin
|img=Sea of Japan Map en.png | pic = Sea of Japan Map en.png
|caption=Tsushima Basin where the ] meets the ] | piccap = Tsushima Basin where the ] meets the ]
⚫ | kanji = 対馬海盆
|koreanname=South Korean name
⚫ | hiragana = つしまかいぼん
⚫ |hangul=울릉분지
| revhep = tsushima kaibon
⚫ |hanja=鬱陵盆地
⚫ | hangul = 울릉분지
|rr= Ulleung Bunji
⚫ | hanja = 鬱陵盆地
|mr= Ulleung Bunchi
| rr = ulleung bunji
|koreantext={{Lang-en|Ulleung Basin}}
| mr = ulleung punji
|sort=japanese2
| ibox-order = ja, ko1, ko4, ko3}}
⚫ |kanji=対馬海盆
⚫ The '''Tsushima Basin''' ({{Langx|ja|対馬海盆|translit=Tsushima kaibon}}) or '''Ulleung Basin''' ({{Korean|hangul=울릉분지|rr=Ulleung bunji}}) is an ] located where the ] meets the ]. It lies immediately south of ] and ], in the eastern end of the ]n ] and the western end of the ]ese EEZ.
⚫ |hiragana=つしまかいぼん
|hepburn=Tsushima Kaibon
|japanesetext={{Lang-en|Tsushima Basin}}


⚫ In 1978, the Japanese government registered the name "Tsushima Basin" with the ]. In April 2006, Japan's plans to survey the region and South Korea's plans to register the name "Ulleung Basin" with the International Hydrographic Bureau resulted in a diplomatic standoff between the two countries. The two countries later agreed to address the issue "at an appropriate time." <ref>{{Cite web|url=http://english.chosun.com/w21data/html/news/200605/200605230014.html|archiveurl=https://web.archive.org/web/20060524034724/http://english.chosun.com/w21data/html/news/200605/200605230014.html|url-status=dead|title=Korea Resumes Project to Name Seabed Near Dokdo|archivedate=May 24, 2006}}</ref>
}}
⚫ The {{nihongo|'''Tsushima Basin'''|対馬海盆|tsushima kaibon}} or '''Ulleung Basin''' (울릉분지 ulleung bunji) is an ] located where the ] meets the ]. It lies immediately south of ] and ], in the eastern end of the ] ] and the western end of the ] EEZ.


⚫ The first exploratory drilling for gas was in 1972, but gas discoveries have drawn regional interest since the late 1980s. The first commercial gas discovery was reported in 1998. Nine of 15 exploratory wells have contained gas, a rate indicating high potential prospects.<ref>{{Cite web |url=http://www.ccop.or.th/epf/korea/korea_petroleum.html |title=Sedimentary Basins, Offshore Korea |access-date=2006-06-06 |archive-date=2007-05-30 |archive-url=https://web.archive.org/web/20070530012437/http://www.ccop.or.th/epf/korea/korea_petroleum.html |url-status=live }}</ref>
⚫ In 1978, the Japanese government registered the name "Tsushima Basin" with the ]. In April 2006, Japan's plans to survey the region and South Korea's plans to register the name "Ulleung Basin" with the International Hydrographic Bureau resulted in a diplomatic standoff between the two countries. The two countries later agreed to address the issue "at an appropriate time." <ref></ref>


⚫ The ], Ulleung Warm Eddy, and Offshore Branch interact within this basin.<ref>{{Cite web |url=http://www.stormingmedia.us/06/0620/A062034.html |title=Decadal Current Variations in the Southwestern Japan/East Sea |access-date=2006-06-06 |archive-date=2007-09-28 |archive-url=https://web.archive.org/web/20070928030139/http://www.stormingmedia.us/06/0620/A062034.html |url-status=live }}</ref>
⚫ The first exploratory drilling for gas was in 1972, but gas discoveries have drawn regional interest since the late 1980s. The first commercial gas discovery was reported in 1998. Nine of 15 exploratory wells have contained gas, a rate indicating high potential prospects. <ref></ref>


⚫ A feature of the southwestern Sea of Japan is a deep, developing ]. The eastern ], a big ridge of three rows lines up in parallel to the Japanese archipelago, and it connects with a ] which has expanded from Oki Islands and offshore of the ] to the south in between those. The vast Tsushima Basin has extended on the tip of the Oki offshore that expands from Oki Islands on the north side.
⚫ The ], Ulleung Warm Eddy, and Offshore Branch interact within this basin. <ref></ref>

⚫ A feature of the southwestern Sea of Japan is a deep, developing ]. The eastern ], a big ridge of three rows lines up in parallel to the Japanese archipelago, and it connects with a ] which has expanded from Oki Islands and offshore of the ] to the south in between those. The vast Tsushima Basin has extended on the tip of the Oki offshore that expands from Oki Islands on the north side.


==References== ==References==
<references/> <references />


==External links== ==External links==
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Latest revision as of 06:21, 28 October 2024

Oceanic Basin in the Sea of Japan

36°34′48.89″N 131°38′57.01″E / 36.5802472°N 131.6491694°E / 36.5802472; 131.6491694

Tsushima Basin
Ulleung Basin
Tsushima Basin where the Sea of Japan meets the Korea Strait
Japanese name
Kanji対馬海盆
Hiraganaつしまかいぼん
Transcriptions
Revised Hepburntsushima kaibon
Korean name
Hangul울릉분지
Hanja鬱陵盆地
Transcriptions
Revised Romanizationulleung bunji
McCune–Reischauerulleung punji

The Tsushima Basin (Japanese: 対馬海盆, romanized: Tsushima kaibon) or Ulleung Basin (Korean: 울릉분지; RR: Ulleung bunji) is an oceanic basin located where the Sea of Japan meets the Korea Strait. It lies immediately south of Ulleung-do and Liancourt Rocks, in the eastern end of the South Korean EEZ and the western end of the Japanese EEZ.

In 1978, the Japanese government registered the name "Tsushima Basin" with the International Hydrographic Bureau. In April 2006, Japan's plans to survey the region and South Korea's plans to register the name "Ulleung Basin" with the International Hydrographic Bureau resulted in a diplomatic standoff between the two countries. The two countries later agreed to address the issue "at an appropriate time."

The first exploratory drilling for gas was in 1972, but gas discoveries have drawn regional interest since the late 1980s. The first commercial gas discovery was reported in 1998. Nine of 15 exploratory wells have contained gas, a rate indicating high potential prospects.

The East Korea Warm Current, Ulleung Warm Eddy, and Offshore Branch interact within this basin.

A feature of the southwestern Sea of Japan is a deep, developing continental shelf. The eastern Oki Islands, a big ridge of three rows lines up in parallel to the Japanese archipelago, and it connects with a Yamato Basin which has expanded from Oki Islands and offshore of the Tōhoku region to the south in between those. The vast Tsushima Basin has extended on the tip of the Oki offshore that expands from Oki Islands on the north side.

References

  1. "Korea Resumes Project to Name Seabed Near Dokdo". Archived from the original on May 24, 2006.
  2. "Sedimentary Basins, Offshore Korea". Archived from the original on 2007-05-30. Retrieved 2006-06-06.
  3. "Decadal Current Variations in the Southwestern Japan/East Sea". Archived from the original on 2007-09-28. Retrieved 2006-06-06.

External links

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