Öz
Bu c;all~rnada, basamak faylaran manyetik ve gravite anomalilerinin yorumu ir;in bir metod sunulmu~cur. Manyetik yorum i<;ill;· d~ey manyetik anomalinin yatay birinci tfilrevinden, gravite yorurnu ic;in ise, gravite anomalisinin yatay ikinci tiirevindcn faydalantlmt~tlr. Manyetik yorum ic;in once, orijin tayini yapthr.' Sonra, yatay birinci tiirev iizerinGravite yorumu ir;in ise, once yatay ikinci tiirev anomalisi iizerinde orijin ta yin edilir. Sonra, bu anomali iizerinde, manyetik yorumdaki gibi, keyfi ii<; adet yatay mesa fo ve bu mesafelere denk gelen ikinci tiirev degerleri tesbit edilir. Bu degerler yard1m1 ile, ii<; adet li~eer de~klem ta~1~1 kurulur. Kuru.~an den~ lem takimtnm r;oziimii 1le elde edtlen degerlerden yararlamlarak, kutleye alt parametreler bulunabilir. ~ail~ma da geli~tirilen y~ntem; bas~r~ak faym, hem manyetik d~ey bile- ~en anomalisene hem de grav1te anomahsme uygulanarak r;ok iyi neticeler elde edilmi~tir. ,>
Öz
An interpretation method has been presented in this work, for magnetic and gravity anomaly of the step faults. The first horizontal derivatives of the vertical magnetic anomaly and the second horizontal derivatives of the gravity anomaly have been used for each interpretation. First of all an origin point has been taken for magnetic interpretation. Than randomly selected five horizontal distances.and their derivatives have been determined on the first horizontal derivative. Thus, five lineer equations have been set up. And finally the mass parameters can be found by means of the solutions of five equations. On the othe.r hand, for interpretation of the gravity data, firstly an origin point have been taken on the second horizontal derivative. Secondly, as . in the magnetic interpretation, three randomly selected horizontal distances and their second derivatives have been determined. Than three Lineer equations have been set up. Thus, the mass parameters can be found by means of the values obtained from the solutions of those three equations. It has been obtained very suitable resolutions· in the magnetic vertical component anomaly and gravity anomaly of the step faults, by using the process developed in this work.
Anahtar Kelimeler
Ayrıntılar
| Birincil Dil | Türkçe |
|---|---|
| Konular | Jeoloji (Diğer) |
| Bölüm | Makaleler |
| Yazarlar | |
| Yayımlanma Tarihi | 16 Ağustos 2014 |
| Yayımlandığı Sayı | Yıl 1985 Cilt: 5 Sayı: 1-2 |