3 edition of The isostatic gravity anomaly field of southwestern Saudi Arabia and its interpretation found in the catalog.
The isostatic gravity anomaly field of southwestern Saudi Arabia and its interpretation
|Statement||by M.E. Gettings ; prepared for the Ministry of Petroleum and Mineral Resources, Deputy Ministry for Mineral Resources, Jiddah, Kingdom of Saudi Arabia.|
|Series||Open-file report -- 85-254., Open-file report (Geological Survey (U.S.)) -- 85-254.|
|Contributions||Saudi Arabia. Deputy Ministry for Mineral Resources., Geological Survey (U.S.)|
|The Physical Object|
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Get this from a library. The isostatic gravity anomaly field of southwestern Saudi Arabia and its interpretation. [M E Gettings; Saudi Arabia. Deputy Ministry Gettings M E The isostatic gravity anomaly field of southwestern Saudi Arabia and its interpretation; Technical Record USGS-TR, Ministry Petrol.
Mineral Resources, Jiddah, Kingdom of Saudi Arabia Anomalies caused by isostatic compensation are mostpronounced in the western part of the area due to the crustal thinning at the Red Sea rift zone.
A regional isostatic gravity field was removed from the Bouguer gravity anomaly by assuming an Airy–Heiskanen model for isostatic compensation of topographic loads (Simpson et al).
The isostatic modeling represents one of the most useful “geological” reduction methods of the gravity field. With the isostatic correction, it is possible to remove a significant part of the effect of deep density heterogeneity, which dominates in the Bouguer gravity anomalies.
Although there exist several isostatic compensation schemes, it is usually supposed that a choice of the model The isostatic gravity anomaly field of southwestern Saudi Arabia and its interpretation by I/ M.
Gettings Open-File Report Prepared for the Ministry of Petroleum and Mineral Resources, Deputy Ministry for Mineral Resources, Jiddah, Kingdom of Saudi Arabia This report is preliminary and has not been reviewed for conformity Gravity field of the Northwest Pacific Ocean Basin and its margin Isostatic and enhanced isostatic gravity anomaly maps of the Arctic L.
Sobczak (State), Pacific Ocean, Saudi Arabia, South Africa, Arizona, Oregon, Antarctica, Brazil, Canada, Southwestern States, Agder, British Columbia, California, Cascade Range The isostatic residual anomaly map is particularly important for geological interpretation in mountainous areas of northern Ethiopia where most low gravity anomalies over high topographic areas were interpreted as only expressions/effects of high topography (e.g.
Oluma and Zewuge, ). In geophysics, the main three anomalies, i.e. the FA anomaly, Bouguer anomaly (BA), and isostatic anomaly (ISA), are distinguished in order to define the gravity field in terms of the height of the observations (e.g., Naudy and Neumann,LaFehr,Li and Götze,Hackney and Featherstone, ; and many others).
FIELD STUDY IN SAUDI ARABIA, FEBRUARY 13 TO MARCH 5, BRGM 1 AEROMAGNETIC AND SCINTILLOMETRIC SHEET NO.BRGM 1 PRELIMINARY MAGNETIC INTRPRETATION SHEET B SCALE Gravity and Magnetic Interpretation Interpretations of GravMag data are non-unique, meaning that sometimes a number of different geological models can fit the observed data.
With constraints from geological and other geophysical data types (e.g. seismic and well data), the interpretations can provide critical insights into the geometry of the Subsurface geometry of Ar Rika and Ruwah faults from gravity and magnetic surveys Article (PDF Available) in Arabian Journal of Geosciences 1(1) July with Reads How we measure Gravity field and isostatic state of Ethiopia and adjacent areas Article in Journal of African Earth Sciences 41() January with 46 Reads How we measure 'reads' A Fast Equivalent Source Technique for Airborne Gravity Gradient Data; A global reference model of the lithosphere and upper mantle from joint inversion and analysis of multiple data sets; Density distribution across the Alpine lithosphere constrained by 3D gravity modelling and relation to A simple Bouguer gravity anomaly map of southwestern Saudi Arabia and an initial interpretation [microfo The isostatic gravity anomaly field of southwestern Saudi Arabia and its interpretation [microform] / by BASIC programs to calculate gravity and magnetic anomalies for 2 1/2-dimensional prismatic bodies [micro Gravity anomaly maps of the British Isles are interpreted as indicating the presence of granite plutons in the following areas.: Also these changes can be presented as gravity anomaly temporal variations.: This anomaly disappears in foals that are the product of an Arabian and another breed of horse.: Santa Cruz, a population located in Remote Oceania, is an anomaly with extreme frequencies of We use long-wavelength free-air gravity anomaly data, taken from Pavlis et al., computed using spherical harmonic coefficients taken from GRACE gravity data ().
Data are filtered in the pass range ≤λ≤ km, and used to construct a 1°× 1° grid. 3 Africa–Arabia The Amar Suture, which marks the collision zone between the Afif terrane and Rayn micro-plate, consists of westerly directed, N-trending thrust faults that contain slices of ophiolite of either oceanic or island-arc origin ().The ophiolites consist of ultramafic rocks, serpentite, gabbro, sheeted dike complexes, theoleitic metabasaltic rocks, and ocean-floor metasedimentary rocks (Brown et al In Saudi Arabia, 12 age determinations of between 2, and 1, Ma (see Figure 2) were published by Aldrich et al.
(), Fleck et al. (), Calvez et al. (, ), Calvez and Delfour (), Stacey and Hedge (), Stacey and Agar (), Stoeser and Stacey (), and Agar et al.
The samples are all from the Al Amar fault Gravity profiles across the Uyaijah Ring structure, Kingdom of Saudi Arabia [microform] / by M.E. Gettings and G.E. Andreasen ; report prepared by the U.S. Geological Survey in cooperation with the Deputy Ministry for Mineral Resources, Saudi Arabia The Survey: [Books and Open-file Reports Section, distributor] [Denver, Colo.?] The gravity station data were reprocessed from observed gravity to simple Bouguer anomaly following standard methods that depend on the station type (for example, land, lake surface, or lake bottom observation) and used a reduction density of 2, kg/m3.
The compilation provides a ?q=&filter=tags=gravitational+field+(earth). A large variation in elevation and gravity anomaly prevails from the Red Sea coast to the interior of the Arabian Shield (AS) across the Asir Igneous Province (AIP); The Asir Mountain (AM) is developed on AIP.
Here the elevation varies from 45 - m, corresponding changes in F.A. are from –30 to + mgal and B.A. from +22 to – :// It is as if some process has caused inelastic flow or ‘freezing’ of the solid rock. Thus, after modification, the central area of the crater becomes super-isostatic.
A large positive free-air gravity anomaly becomes locked in, probably because of an uplifted Moho and upper mantle that is locked into place. These are called mascons. 42Effective elastic thickness (EET) of the lithosphere is the thickness of a uniform elastic layer that would respond to applied loads in the same way as the heterogeneous lithospheric plate.
EET primarily depends on thermal state and structure of the lithosphere [e.g., Burov and Diament, ]; therefore, this parameter can be directly used to