Results 111 to 120 of about 7,304 (232)

The geology and geophysics of the Oslo rift [PDF]

open access: yes
The regional geology and geophysical characteristics of the Oslo graben are reviewed. The graben is part of a Permian age failed continental rift. Alkali olivine, tholefitic, and monzonitic intrusives as well as basaltic lavas outline the extent of the ...
Ruder, M. E.
core   +1 more source

Gravimetric maps of the Central African Republic [PDF]

open access: yes
Gravimetric maps of the Central African Republic are described including a map of Bouguer anomalies at 1/1,000,000 in two sections (eastern sheet, western sheet) and a map, in color, of Bouguer anomalies at 1/2,000,000. Instrumentation, data acquisition,
Albouy, J., Godivier, R.
core   +1 more source

Satellite and surface geophysical expression of anomalous crustal structure in Kentucky and Tennessee [PDF]

open access: yes
An equivalent layer magnetization model is discussed. Inversion of long wavelength satellite magnetic anomaly data indicates a very magnetic source region centered in south central Kentucky.
Mayhew, M. A.   +2 more
core   +1 more source

Geological Structure Analysis of Satellit Gravity Data in Oil and Gas Prospect Area of West Aceh-Indonesia

open access: yesJournal of Aceh Physics Society, 2019
Estimation of the subsurface geological structures in oil and gas prospect area of West Aceh has been done by utilizing gravity field anomaly of satellite gravity data.
Dian Darisma   +2 more
doaj  

Shuttle imaging radar-A (SIR-A) data analysis [PDF]

open access: yes
The utility of shuttle imaging radar (SIR-A) data was evaluated in several geological and environmental contexts. For the Ozark Plateau of southern Missouri, SIR-A data were of little use in mapping structural features, because of generally uniform ...
Arvidson, R. E.
core   +1 more source

Investigation of lunar crustal structure and isostasy [PDF]

open access: yes
The lunar mascon basins have strongly free air gravity anomalies, generally exceeding 100 milligals at an elevation of 100 km. The source of the anomalies is a combination of mantle uplift beneath the impact basins and subsequent infilling by high ...
Thurber, Clifford H.
core   +1 more source

Home - About - Disclaimer - Privacy