Within the framework of LOREX experiment the mineral Lorandite (TlAsS2
) of the old (5 x 10(6) years) arsenic mine Allchar (Kavadarci, Macedo
nia) will be used to estimate average solar neutrino flux from the amo
unts of Pb-205 isotope (T1/2 = 1.5 x 10(7) years) induced by Tl-205 (n
u(e), e-) Pb-205 reaction. In order to evaluate the amount' of the Pb-
205 isotope induced by Pb-204 (n, gamma) Pb-205 reaction the thermal n
eutron flux inside and above the mine was measured by our high sensiti
ve etched track neutron dosemeters (CR-39/BE, CR-39/BN-1). The thermal
neutron flux was found to be (2.7 +/- 0.4) x 10(-3) cm-2 s-1. In addi
tion to cosmic muon interactions and spontaneous fissions the neutrons
can be produced through various (alpha, n) reactions due to the high
alpha particle flux from the decay chains of uranium and thorium. Ther
efore radon concentration in the mine was measured by our diffusion ch
amber type dosemeter utilizing CR-39 detector and was found to be 1.5
x 10(4) Bq m-3. The possibilities to extend the application of etched
track detectors to another solar neutrino experiments are discussed.