Geophysical investigations of a geothermal anomaly at Wadi Ghadir, eastern Egypt [PDF]
During regional heat flow studies a geothermal anomaly was discovered approximately 2 km from the Red Sea coast at Wadi Ghadir, in the Red Sea Hills of Eastern Egypt.
Basta, N. Z. +6 more
core +1 more source
Geothermal field "X" is one of the geothermal fields located in North Sulawesi Province managed by PT Pertamina Geothermal Energy. This research aims to determine the presence of geothermal system components in the subsurface using the gravity method ...
Mochammad Malik Ibrahim +2 more
doaj +1 more source
Un modelo geodésico para Colombia
<p class="MsoNormal" style="line-height: normal; margin: 0cm 0cm 0pt; mso-layout-grid-align: none;"><span style="font-family: ";Arial";,";sans-serif";; font-size: 12pt; mso-ansi-language: EN-US;" lang="EN-US">The processed gravimetric ...
Sánchez Rodríguez Laura Marlene +2 more
doaj
Magyarország Bouguer-anomália térképének frekvenciatartománybeli vizsgálata és értelmezése = Investigation of spectral domain, and interpretation of Bouguer anomaly map of Hungary [PDF]
Ez a harmadik cikkünk a kétdimenziós spektrálanalízis témakörében. Most a magyarországi gravitációs Bougueranomáliatérképét vizsgáljuk. A Magyar Geofi ziká.ban közölt egyik előző cikkben a Kárpát-Pannon térség területét, azaz az országhatárokon ...
Kiss, János
core
The Mount Jonggol region in Kulon Progo, Yogyakarta, constitutes an important segment of the Sunda–Banda magmatic arc system; however, its subsurface structural configuration remains insufficiently understood.
Setyo Pambudi +2 more
doaj +1 more source
Gravity survey of the Mt. Toondina impact structure, South Australia [PDF]
The Mt. Toondina impact structure is located in northern South Australia, about 45 km south of the town of Oodnadatta. Only the central uplift is exposed. The outcrops at Mt.
Plescia, J. B. +2 more
core +1 more source
Reliability of Assessing Lunar Crustal Density Structures Using the GRAIL Gravity Model
The spatial resolution of gravity data acquired by the Gravity Recovery and Interior Laboratory (GRAIL) mission is adequate to resolve relatively small-scale density structures larger than approximately tens of kilometers within the lunar crust, which ...
Qingyun Deng, Zhiyong Xiao, Fei Li
doaj +1 more source
Comparisons of global topographic/isostatic models to the Earth's observed gravity field [PDF]
The Earth's gravitational potential, as described by a spherical harmonic expansion to degree 180, was compared to the potential implied by the topography and its isostatic compensation using five different hypothesis.
Rapp, Richard H. +3 more
core +1 more source
Properties of the lithosphere and asthenosphere deduced from geoid observations [PDF]
Data from the GEOS-3 and SEASAT Satellites provided a very accurate geoid map over the oceans. Broad bathymetric features in the oceans such as oceanic swells and plateaus are fully compensated.
Turcotte, D. L.
core +1 more source
Petrologic model of the northern Mississippi embayment based on satellite magnetic and ground based geophysical data [PDF]
Magnetization, derived from gravity-seismic data from the northern Mississippi Embayment, is evaluated relative to magnetization values obtained from satellite magnetic data.
Thomas, H. H.
core +1 more source

