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Pregled bibliografske jedinice broj: 466478

Estimation of the normal geomagnetic field and geological interpretation of the normal field anomalies over middle-northern Croatia


Vujić, Eugen; Verbanac, Giuliana; Frančišković-Bilinski, Stanislav; Vujnović, Vladis; Marki, Antun
Estimation of the normal geomagnetic field and geological interpretation of the normal field anomalies over middle-northern Croatia // Studia geophysica et geodaetica, 55 (2011), 1; 175-190 doi:10.1007/s11200-011-0010-9 (međunarodna recenzija, članak, znanstveni)


Naslov
Estimation of the normal geomagnetic field and geological interpretation of the normal field anomalies over middle-northern Croatia

Autori
Vujić, Eugen ; Verbanac, Giuliana ; Frančišković-Bilinski, Stanislav ; Vujnović, Vladis ; Marki, Antun

Izvornik
Studia geophysica et geodaetica (0039-3169) 55 (2011), 1; 175-190

Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni

Ključne riječi
Ground total-field data; normal geomagnetic field; geological interpretation of geomagnetic anomalies

Sažetak
Based on the ground survey of total-field magnetic data at 53 sites, which recorded a time-series over the interval 2003-2005, the core field + long wavelength lithospheric field over the middle-northern Croatia region was calculated. The dimension of the survey was 18, 900 km2, and an average distance between the neighbouring sites being 12 km. The results were reduced to 2004.5 epoch. This “normal” total-field was estimated using the first-order Taylor polynomial as a function of geographic coordinates, and the polynomial coefficients were calculated with three methods of adjustment: simple and weighted least squares fits and adjustment according to the most frequent value. The stability of the normal field was tested using the Monte Carlo-type test, by decreasing the input data set in each adjustment (up to 90%). All obtained field residuals (measured-“normal”) were mutually compared, as well as fit coefficients of the Taylor polynomials. The residual values indicate the presence of shorter-wavelength anomalies, i.e. the three major residual anomalies were found (-106 nT, 74 nT and 57 nT). The geostatistical analysis of the ground survey data and the normal field residuals (respectively), using the median absolute deviation method, was further conducted in order to evaluate the calculated anomalies. The geological situation around the anomalies derived by the median absolute deviation method, and around the normal field residual anomalies, is given. The correlation was found between higher value anomalies of the normal field residuals, and shallow volcanic rocks and oil field, respectively.

Izvorni jezik
Engleski

Znanstvena područja
Geologija



POVEZANOST RADA


Projekt / tema
098-0982934-2720 - MEĐUDJELOVANJA OBLIKA TRAGOVA METALA U VODENOM OKOLIŠU (Ivanka Pižeta, )
119-1193086-1314 - Istraživanje geomagnetskog polja i nehomogenosti litosfere u području Hrvatske (Davorka Herak, )

Ustanove
Institut "Ruđer Bošković", Zagreb,
Prirodoslovno-matematički fakultet, Zagreb

Časopis indeksira:


  • Current Contents Connect (CCC)
  • Web of Science Core Collection (WoSCC)
    • Science Citation Index Expanded (SCI-EXP)
    • SCI-EXP, SSCI i/ili A&HCI
  • Scopus


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