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The Compton–Belkovich Thorium Anomaly is a hotspot (volcanic complex) on the Moon. It is on the far side of the Moon and was found by a gamma-ray spectrometer in 1998. It is an area of concentrated thorium, a 'fertile' element. Lunar rock samples from the Apollo missions reveal that most lunar volcanism occurred around 3 to 4 billion years ago, but this feature could have formed as recently as 1 billion years ago due to the unknown history of the moon's far side.

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  • Compton–Belkovich Thorium Anomaly (en)
  • Anomalia de Compton-Belkovich (ca)
  • Compton-Belkovich-Thoriumanomalie (de)
  • Anomalía de Compton-Belkovich (es)
  • Anomalie de Compton-Bel'kovich (fr)
  • 컴튼-벨코비치 토륨 이상 (ko)
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  • L'anomalia de Compton Belkovich és un punt calent (conjunt volcànic) al costat ocult de la Lluna. Fou trobat per un espectròmetre de radiació gamma al 1998. És una àrea de concentració de tori, un element radioactiu. Les mostres de roques lunars del programa Apollo revelaren que la majoria del vulcanisme lunar s'havia produït fa uns de 3.000 a 4.000 milions anys, però podria haver sigut més recent, fa uns mil milions d'anys, a causa de la història desconeguda del costat ocult de la Lluna. (ca)
  • Die Compton-Belkovich-Thoriumanomalie ist ein Hotspot (vulkanischer Komplex) auf der erdabgewandten Seite des Mondes. Sie wurde 1998 mit Hilfe des Lunar Prospectors entdeckt. In dieser Region herrscht eine hohe Konzentration des schwach radioaktiven Elements Thorium. Aufgrund der Gesteinsproben aus den Apollo-Missionen wurde bis dahin davon ausgegangen, dass der Vulkanismus auf dem Mond vor drei bis vier Milliarden Jahren seinen Höhepunkt erreicht hatte. Dabei deuten nun diese Ergebnisse auf deutlich jüngere vulkanische Aktivitäten vor ca. einer Milliarde Jahren auf der Mondrückseite hin. (de)
  • The Compton–Belkovich Thorium Anomaly is a hotspot (volcanic complex) on the Moon. It is on the far side of the Moon and was found by a gamma-ray spectrometer in 1998. It is an area of concentrated thorium, a 'fertile' element. Lunar rock samples from the Apollo missions reveal that most lunar volcanism occurred around 3 to 4 billion years ago, but this feature could have formed as recently as 1 billion years ago due to the unknown history of the moon's far side. (en)
  • La anomalía de Torio-Compton Belkovich es un punto caliente (complejo volcánico) en el lado oculto de la Luna . Fue encontrado por medio de un espectrómetro de rayos gamma en 1998.​ Es un área de concentración de torio , un elemento radiactivo.​ Las muestras de rocas lunares de las misiones Apolo revelaron que la mayoría del vulcanismo lunar se produjo hace alrededor de 3000 a 4000 millones años, pero podría haber sido más reciente, como hace mil millones de años, debido a la historia desconocida del lado oculto de la Luna. (es)
  • 컴튼-벨코비치 토륨 이상(Compton–Belkovich Thorium Anomaly)은 달의 뒷면에 있는 열점(복합 화산)으로, 1998년 감마선 분광기를 이용한 관측에서 발견하였다. 이 지역에는 핵원료 물질인 토륨이 풍부하다. 아폴로 계획에서 채취한 월석 표본 분석에서는 달에서의 화산 활동이 30억~40억 년 전에 일어난 것으로 밝혀졌지만, 달의 뒷면에 대해 밝혀진 것이 부족하기 때문에 컴튼-벨코비치 토륨 이상의 형성 시기는 10억 년 전까지 올라올 수도 있을 것으로 추정하고 있다. (ko)
  • L'anomalie de Compton-Bel'kovich (en anglais : Compton–Belkovich Thorium Anomaly, CBTA) est une zone de la surface lunaire particulièrement riche en thorium, détectée en 1998 par le spectromètre gamma de la sonde Lunar Prospector. Cette zone se trouve sur la face cachée de la Lune, entre les cratères d'impact (en) (103.8°E, 55.3°N) et Bel'kovich (90.2°E, 61.1°N). C'est le seul exemple sur la Lune où une anomalie en thorium est corrélée à une anomalie d'albédo (photographie ci-contre). (fr)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Compton-Belkovich_Thorium_Anomaly.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Compton-Belkovich_Thorium_Anomaly.png
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