دراسة التمغنط الموجه للرسوبيات الاصطناعية، وتصحيح خطأ ميله
العنوان باللغة الأجنبية:
A Study of Guided Magnetism for Artificial Sediments and a Correction of its Declination Error
المجال العلمي:
العلوم الأساسية
الكاتب:
د. لؤي محمد
العدد:
2
المجلد:
30
السنة:
2008
الملخّص
لمحة عن المقال باللغة الأجنبية:
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: 1. The component of oriented and thermal magnetism of sedimentary and igneous rocks maintains a fixed value in the direction of the ground magnetic field. 2. A study of rock magnetism allows us to understand the internal structure of the earth by identifying the minerals present in rocks. 3. 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 rock
s.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: 1. The component of oriented and thermal magnetism of sedimentary and igneous rocks maintains a fixed value in the direction of the ground magnetic field. 2. A study of rock magnetism allows us to understand the internal structure of the earth by identifying the minerals present in rocks. 3. 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 rock
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