GEOPHYSICAL EXPLORATION AND DISCOVERY OF THE BUDAFAPUSZTA (LISPE) OIL FIELD IN HUNGARY

Geophysics ◽  
1947 ◽  
Vol 12 (2) ◽  
pp. 208-220 ◽  
Author(s):  
D. C. Skeels ◽  
Raoul Vajk

Interest was first attracted to the Budafapuszta area by its geographical position on the eastward projection of a known surface anticline, which had produced small quantities of oil at Peklenicza and Szelnicza. A test was located in 1920 on a small surface feature, and completed in 1923 as a dry hole. In 1934 a torsion balance survey was made by Eurogasco, a subsidiary of the Standard Oil Co. (N. J.) which indicated a dome with its crest 1500 m. north of the dry hole. A reflection survey verified the presence of the structure. The discovery well was located by the torsion balance data, and completed as a producer in 1937. A gravity meter survey made after the first two producers had been drilled, gave further information on the structure and assisted in the development of the field. This exploration history shows that a properly made torsion balance survey may be very efficient and economical even in hilly country. A geological map of part of the Szelnicza‐Peklenicza anticline, a topographical map, torsion balance, seismograph and gravity meter maps, a seismograph cross section and a subsurface contour map of the Budafapuszta structure are submitted.

Wahana Fisika ◽  
2017 ◽  
Vol 2 (1) ◽  
pp. 1 ◽  
Author(s):  
Jamaludin Hasibuan ◽  
Asdiati Berutu ◽  
Halimahtun Sakdiah ◽  
Rahmatsyah Rahmatsyah

Penelitian penentuan anomali magnetik situs arkeologi di Tapanuli Tengah dengan metode geomagnetik telah dilakukan untuk mengetahui adanya penampang anomali magnetik di lokasi Lobu Tua. Metode pengukuran Geomagnet menggunakan tipe PPM (Proton Precession Magnetometer) Elsec 770, pengambilan data dilakukan secara acak dengan jumlah titik yang diperoleh 51 titik pengukuran, pengolahan data menggunakan surfer 11 untuk mendapatkan peta kontur dan Mag2DC for windows. Hasil penelitian menunjukkan bahwa penyebaran struktur pelapis Lobu Tua menggunakan metode geomagnet menyebar secara vertikal dan horizontal. Anomali dengan metode geomagnetik memiliki nilai terendah - 122,34 nT dan nilai tertinggi adalah -100,34 nT, dan nilai suseptibilitas 0,77, 0,87, 0,91 dimana model anomali permukaan didominasi oleh batuan alluvium sesuai dengan Peta geologi.Research on the determination of anomaly archaeological site in Central Tapanuli by geomagnetic method has been done in order to know the magnetic anomaly cross section of Lobu Tua site. Geomagnet measurement method using PPM (Proton Precession Magnetometer) type Elsec 770, data retrieval is done randomly with number of point obtained 51 point measure, data processing using surfer 11 to get contour map and Mag2DC for windows. The result of the research shows that the dissemination of Lobu Tua's site coating structure using geomagnet method is spread vertically and horizontally. The anomaly with geomagnetic method has the lowest value - 122,34 nT and the highest value is -100,34 nT, and the susceptibility value 0,77, 0,87, 0.91 where the surface anomaly model is dominated by alluvium rocks according to the geological map.


Geophysics ◽  
1947 ◽  
Vol 12 (2) ◽  
pp. 191-199
Author(s):  
Glenn E. Bader

Early geophysical exploration in the Anahuac area from 1925 to 1929 included refraction fan shooting and a torsion balance survey. A reflection dip survey in 1933 indicated a large structural closure on which the discovery well was drilled in 1935. No detailed geophysical work has been done on the structure since the discovery of the field.


1952 ◽  
Author(s):  
Charles Edgar Erdmann ◽  
B.K. Koskinen
Keyword(s):  

Geophysics ◽  
1947 ◽  
Vol 12 (1) ◽  
pp. 13-29
Author(s):  
Holland McCarver ◽  
Lloyd G. West

The Odem field, located in southern San Patricio County, Texas, was discovered in the latter part of 1939. Prior to 1933, the Odem area received a limited amount of geological and geophysical exploration, and several test wells were drilled. These tests were dry and the area apparently condemned until a reflection seismograph survey indicated structure. Subsequent drilling confirmed the presence of a structure containing several producing horizons. The proven limits of production conformed closely to the contours of the original seismograph map.


Geophysics ◽  
1945 ◽  
Vol 10 (1) ◽  
pp. 1-16
Author(s):  
Glenn M. McGuckin

In order to demonstrate the growth of our knowledge of a typical Gulf Coast salt dome concurrently with development of the science of geophysics, the successive application of various techniques to the exploration of the Cameron Meadows dome is described and illustrated. These methods were: mechanical refraction seismograph (1926); torsion balance (1927); electrical refraction seismograph (1928–29); early correlation reflection seismograph (1929); dip reflection seismograph (1933); special salt profiling refraction seismograph (1942); continuous correlation reflection seismograph (1942); gravity meter (1943.)


Geophysics ◽  
1952 ◽  
Vol 17 (2) ◽  
pp. 278-310 ◽  
Author(s):  
Raoul Vajk

Geophysical exploration of an eight million acre oil concession covering southwest Hungary is discussed. During ten years of exploration (1933–1943), about 20,000 torsion balance, 12,000 gravity meter, and 15,000 magnetometer stations were made, and reflection seismograms were recorded at about 2,500 shot points. As a result of this exploration, four oil pools and a gas pool were discovered and a number of geological structures and major faults were located. Gravity, magnetic, and seismic maps showing most of the geophysical data are submitted. Interpretations of the geophysical results, geological data from subsequent drilling, and a schematic tectonic map of southwest Hungary based on the geophysical surveys are also presented.


1977 ◽  
Vol 99 (2) ◽  
pp. 367-373 ◽  
Author(s):  
B. H. Walker ◽  
M. B. Friedman

A mathematical model of an oil field drill string which includes the effect of torque has been developed. The drill string can include arbitrary members with known mechanical properties. The solution gives the three-dimensional deflection curve, forces on the borehole wall, the magnitude and direction of the resultant force and slope of the deflection curve at the bit.


1922 ◽  
Vol 59 (4) ◽  
pp. 146-156 ◽  
Author(s):  
Reginald A. Daly

The writings of Charles Darwin, Renard, Mellis, Reinisch, and others have already made the salient features of lonely Ascension and St. Helena accessible, if not familiar, to geologists— St. Helena has won the surprised interest of biologists, who have long speculated on the origin of its unique species of plants and animals. From each island collections of rocks have been made. Following Renard's well-known contribution to the petrography of Ascension (“Challenger” Reports, Physics and Chemistry, vol. ii, 1889), Reinisch's paper in the Report of the Deutsche Siidpolar Expedition (1901–3) gives a large number of petrographical. descriptions, including a goodly number of chemical analyses. No adequate geological map of either island has, however, been published, nor, indeed, was this really possible before the British Admiralty had issued the greatly improved chart (No. 1691) of Ascension, in 1910, with corrections added to the year 1921, and the British War Office had issued its excellent contour-map of St. Helena, dated 1904. Each map is on a large scale. Even, though lacking contour lines, the Ascension chart was obviously to be of service to anyone attempting a reconnaisance survey of that island.


1991 ◽  
Vol 10 (1) ◽  
pp. 38-43 ◽  
Author(s):  
Peter Roper

William Barton Rogers' pioneering geological survey was terminated in 1842 with none of its three principal aims accomplished. In particular no funds were made available for the preparation of a geological map, even supposing that a suitable base map existed for the purpose. Thirty-four years were to elapse before Jedediah Hotchkiss, appointed by Virginia's Board of Immigration to write a wide-ranging geographical and political description of Virginia, produced a topographical map at a scale of 24 miles to one inch on which Rogers was able to delineate the results of the survey. Later, Hotchkiss publicized Rogers' work in the mining and scientific journal, The Virginias, which he founded in 1880. In the June issue of that year he included a version of this geological map. Later, Rogers and Hotchkiss planned to produce a new map at a scale of 8 miles to one inch. Following the death of Rogers in 1882, Hotchkiss collaborated with Emma Rogers in preparing a reprint of Rogers' survey reports and other papers relating to the geology of Virginia; this was to be accompanied by the larger scale map. In the event, Hotchkiss was only able to provide a revisision of the 1880 map. However, he did edit and supervise the printing of the 96 sections produced by Rogers. These were exhibited at the New Orleans Exposition 1884/5 along with the new edition of the 24 miles to one inch map. He also displayed wall maps of Virginia at a scale of 3.5 miles to one inch, including one showing Rogers' geology.


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