Магнито-геологическая модель золотого оруденения в пологозалегающих структурах на примере месторождения Чертово Корыто (Байкало-Патомское нагорье); Глубинное строение, геодинамика, тепловое поле земли, интерпретация геофизических полей
| Parent link: | Глубинное строение, геодинамика, тепловое поле земли, интерпретация геофизических полей.— 2011.— [С. 187-190] |
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| Prif Awdur: | |
| Awduron Eraill: | , |
| Crynodeb: | Заглавие с экрана The anomalous properties of the rocks are determined by pyrrhotine occurrence which isone of the basic minerals of ore assemblage. The effect of demagnetization causes magneticanisotropy of rocks and results in a close association of magnetization direction with orientation ofsulphade bands. Multidirectional magnetization determined the magnetic field structure as asuperposition of areal dipole and a set of local linear anomalies arising from sulphide occurrenceswhich constitute shallow and steeply dipping disjunctive dislocations. |
| Iaith: | Rwseg |
| Cyhoeddwyd: |
2011
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| Pynciau: | |
| Mynediad Ar-lein: | http://www.igeoph.net/Seminary/bulash2011/bulashevich_6.pdf#page=188 |
| Fformat: | Electronig Pennod Llyfr |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=653388 |
| Crynodeb: | Заглавие с экрана The anomalous properties of the rocks are determined by pyrrhotine occurrence which isone of the basic minerals of ore assemblage. The effect of demagnetization causes magneticanisotropy of rocks and results in a close association of magnetization direction with orientation ofsulphade bands. Multidirectional magnetization determined the magnetic field structure as asuperposition of areal dipole and a set of local linear anomalies arising from sulphide occurrenceswhich constitute shallow and steeply dipping disjunctive dislocations. |
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