Tishreen University ournal for Research and Scientific Studies - Basic Sciences Series Vol. No. * *
Tishreen University ournal for Research and Scientific Studies - Basic Sciences Series Vol. No. A Study of Guided Magnetism for Artificial Sediments and a Correction of its Declination Error L. Mohammed * Dr. Loui Mohammed * Received ١١ / ١١ / ٢٠٠٨. Accepted ٩/٥/٢٠٠٨ ABSTRACT Physical properties in geology are based on understanding the nature and characteristics of rock magnetism guided and thermal magnetism of sedimentary and igneous rocks for several reasons, namely:. The component of oriented and thermal magnetism of sedimentary and igneous rocks maintains a fixed value in the direction of the ground magnetic field.. A study of rock magnetism allows us to understand the internal structure of the earth by identifying the minerals present in rocks.. The magnetic excavation of mineral resources in the depth of earth depends on studying the component of guided magnetism, where magnetic abnormality is specially connected with rocks containing some magnetic materials. This research aims at studying the physical properties of guided magnetism for artificial sediments whose area of sedimentary basins are so big in order to approach this study from the natural conditions responsible for forming sedimentary rocks. Keywords: orientation magnetism, synthetic deposition, error of guided magnetism * Lecturer at Physics Department, Faculty of Science, Tishreen University, Lattakia - Syria * Assistant Professor, Physics Department, Faculty of Science, Tishreen University, Lattakia, Syria.
Tishreen University ournal. Bas Sciences Series Orientation magnetization H Magnetic materials m m Fe O Ferromagnetism Hematit Fe O Magnetit Magnetic field ohnson Nagata m i Thermal.magnetization m i t H Khramov Belacone-Shashkanov theory of claster Belacone-Shashkanov
H Paleomagnetizm Primary.magnetization Inclination 0 o o 0 Error of Inclination 0 0 tg f tg 0 f 1 f arcsin cos sin f 0 0 Secondary magnetization Chemistry magnetization
Tishreen University ournal. Bas Sciences Series King Anisotropy Index z x z 0 x x p / z d ro ro p d ctg p ctg 1 1 0 d Remnant deposition rd DRM PDRM rpd DRM PDRM ro rd rpd
x, y, z O O O H T H T North x OA SGF East component y OA component Vertical.component z OA
Tishreen University ournal. Bas Sciences Series x O D H B y H T A z >> H Horizontal component OA The magnetic Meridian Plane OB ob ˆ AoB ˆ Declination D Inclination D H T H T H D Elements of the geometric field H cos D, H sin D, H tg 2 2 2 2 2 2 H HT H D H H sin cosec T,, tg 0
cm m Synthetical deposition kg kg kg F O g g Fe O m letter kg Fanzulaw O cm kg cm
Tishreen University ournal. Bas Sciences Series cm O O O anovsky Magnetometer Ion - التدرجی ة/ 0.12 6 التدرجی ة/ 310 o 73 1.0 Oe 79.6 A/m 0.5Oe 40 A/m Oe - H hor. -
O
Tishreen University ournal. Bas Sciences Series 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 H hor. 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 0 D O O o 90 H 0.54Oe 79.6 A/m Oe H
o 90 - - - - - - - - -
Tishreen University ournal. Bas Sciences Series H H H 0.0Oe H 0.0Oe -
PDRM ro O
Tishreen University ournal. Bas Sciences Series D 0 O n D H tg tg 0 ro ro ro ro tg 0 tg tg ro ro ro ro ro min O ro
o arctg O ro min a 419 320 z 370 2 b max min 872 471 400 z ro ro 400 370 z 385 2 O 978 O c 978 385 arctg 71 471 o o i O O i ro i min ro ro i D D D max
Tishreen University ournal. Bas Sciences Series D max 0 n cos D, sin D, tg ro n max n max O n 0 a b Ferromagnetism D DRM: Deposition Remnant Magnetization PDRM: Post Deposition Remnant magnetization SGF: Strength of the Geomagnetic Field
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