Exposure histories of the lunar meteorites: MAC88104, MAC88105, Y791197, and Y86032

TY - JOUR

T1 - Exposure histories of the lunar meteorites

T2 - MAC88104, MAC88105, Y791197, and Y86032

AU - Vogt, S.

AU - Fink, D.

AU - Klein, J.

AU - Mlddleton, R.

AU - Dockhorn, B.

AU - Korschinek, G.

AU - Nolte, E.

AU - Herzog, G. F.

PY - 1991/11

Y1 - 1991/11

N2 - Four lunar meteorites, MacAlpine Hills (MAC) 88104, MacAlpine Hills 88105, Yamato (Y) 791197, and Yamato 86032 were analyzed for the cosmogenic radionuclides 10Be, 26Al, 36Cl, and 41Ca. From these and published data, histories of exposure to cosmic rays were modelled in terms of two-stage irradiations each with a long first stage on the Moon lasting a time T2π > 5 Ma at a burial depth d2π[ g cm2] followed by a second stage in space, i.e., the transit time between the Moon and the Earth, lasting a time T4π [Ma] in a body of typical meteoroidal size. The terrestrial age Tt [Ma]gives the time elapsed between meteorite fall and recovery in Antarctica. The following sets of parameters were obtained: MAC88104/5, 390 ≤ d2π ≤ 500, 0.04 ≤ T4π ≤ 0.11, 0.10 ≤ Tt ≤ 0.19; Y791197, d2π < 80, T4π < 0.1, Tt < 0.1; Y86032, d2π > 1000, T4π = 10 ± 2, 0.08 < Tt < 0.12. From the number and exposure histories of lunar meteorites we infer a production rate on the order of 5 Ma-1 and an arrival rate worldwide of about 3 × 106 meteorites Ma-1. These results suggest that each impact event large enough to produce lunar meteorites sends a large number of them to the Earth.

AB - Four lunar meteorites, MacAlpine Hills (MAC) 88104, MacAlpine Hills 88105, Yamato (Y) 791197, and Yamato 86032 were analyzed for the cosmogenic radionuclides 10Be, 26Al, 36Cl, and 41Ca. From these and published data, histories of exposure to cosmic rays were modelled in terms of two-stage irradiations each with a long first stage on the Moon lasting a time T2π > 5 Ma at a burial depth d2π[ g cm2] followed by a second stage in space, i.e., the transit time between the Moon and the Earth, lasting a time T4π [Ma] in a body of typical meteoroidal size. The terrestrial age Tt [Ma]gives the time elapsed between meteorite fall and recovery in Antarctica. The following sets of parameters were obtained: MAC88104/5, 390 ≤ d2π ≤ 500, 0.04 ≤ T4π ≤ 0.11, 0.10 ≤ Tt ≤ 0.19; Y791197, d2π < 80, T4π < 0.1, Tt < 0.1; Y86032, d2π > 1000, T4π = 10 ± 2, 0.08 < Tt < 0.12. From the number and exposure histories of lunar meteorites we infer a production rate on the order of 5 Ma-1 and an arrival rate worldwide of about 3 × 106 meteorites Ma-1. These results suggest that each impact event large enough to produce lunar meteorites sends a large number of them to the Earth.

UR - https://www.scopus.com/pages/publications/0026287377

UR - https://www.scopus.com/pages/publications/0026287377#tab=citedBy

U2 - 10.1016/0016-7037(91)90480-S

DO - 10.1016/0016-7037(91)90480-S

M3 - Article

SN - 0016-7037

VL - 55

SP - 3157

EP - 3165

JO - Geochimica et Cosmochimica Acta

JF - Geochimica et Cosmochimica Acta

IS - 11

ER -