Cross section of the<mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" display="inline"><mml:mmultiscripts><mml:mi mathvariant="normal">C</mml:mi><mml:mprescripts/><mml:none/><mml:mrow><mml:mn>13</mml:mn></mml:mrow></mml:mmultiscripts></mml:math>(<mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" display="inline"><mml:mrow><mml:mi>α</mml:mi><mml:mo>,</mml:mo><mml:mi>n</mml:mi></mml:mrow></mml:math>)<mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" display="inline"><mml:mmultiscripts><mml:mi mathvariant="normal">O</mml:mi><mml:mprescripts/><mml:none/><mml:mrow><mml:mn>16</mml:mn></mml:mrow></mml:mmultiscripts></mml:math>reaction: A background for the measurement of geo-neutrinos
S. Harissopulos(Institute of Nuclear and Particle Physics), F. Strieder(Ruhr University Bochum), C. Rolfs(Ruhr University Bochum), A. Lagoyannis(National Centre of Scientific Research "Demokritos"), Harry Becker(Ruhr University Bochum), J. W. Hammer
Cited by 115
Related Papers
Highly siderophile element composition of the Earth’s primitive upper mantle: Constraints from new data on peridotite massifs and xenoliths
|Geochimica et Cosmochimica Acta|2006|599
Comparative 187Re-187Os systematics of chondrites
|Geochimica et Cosmochimica Acta|2002|285
Trace element fractionation during dehydration of eclogites from high-pressure terranes and the implications for element fluxes in subduction zones
|Chemical Geology|2000|275
Rhodium, gold and other highly siderophile element abundances in chondritic meteorites
|Geochimica et Cosmochimica Acta|2009|232