A geophysical survey using gravity method was conducted at Bukit Bunuh, Lenggong, Perak, Malaysia, to determine the occurrence of a subsurface impact crater, based on the discovery of meteorite impact rock, suevite, in the study area. A standard correction was applied to all the gravity data to produce Bouguer gravity anomaly of the study area. The Bouguer gravity anomaly was used to produce several maps of gravity anomalies by filtering processes and relate them to the geological structure and tectonic history of the study area. Data processing and interpretation were conducted using geophysical software, Oasis Montaj. This software was used in a number of gravity data filtering processes, such as Low Pass Filter (LPF) and the Total Horizo...
Gravity anomalies can yield an indirect but extremely useful picture of lateral changes in rock comp...
-Geophysics investigation with the gravity method to antisipate the existence of boundary of North ...
A gravity survey was carried out in the middle of 1988 to determine the structure of the Layang-Laya...
A geophysical survey using gravity method was conducted at Bukit Bunuh, Lenggong, Perak, Malaysia, t...
Analyses and interpretation of magnetic and gravity fields data acquired at Bukit Bunuh, Lenggong, P...
The identification and discovery of meteorite impact structures are based on several observation on ...
The aim of gravity survey is to assist in the detection and delineation of subsurface geological fea...
Forward modeling is commonly applied to gravity field data of impact structures to determine the mai...
Geophysical surveys were conducted in Bukit Bunuh area, Perak to study an hypothesis of the existenc...
Forward modeling is commonly applied to gravity field data of impact structures to determine the mai...
Forward modeling is commonly applied to gravity field data of impact structures to determine the mai...
Forward modeling is commonly applied to gravity field data of impact structures to determine the mai...
Alluvial tin mining in Karangan area was closely related to the mineralization of Bongsu Granite and...
Gravity survey is one of the passive geophysical techniques commonly used to delineate geological fo...
Gravity anomalies can yield an indirect but extremely useful picture of lateral changes in rock comp...
Gravity anomalies can yield an indirect but extremely useful picture of lateral changes in rock comp...
-Geophysics investigation with the gravity method to antisipate the existence of boundary of North ...
A gravity survey was carried out in the middle of 1988 to determine the structure of the Layang-Laya...
A geophysical survey using gravity method was conducted at Bukit Bunuh, Lenggong, Perak, Malaysia, t...
Analyses and interpretation of magnetic and gravity fields data acquired at Bukit Bunuh, Lenggong, P...
The identification and discovery of meteorite impact structures are based on several observation on ...
The aim of gravity survey is to assist in the detection and delineation of subsurface geological fea...
Forward modeling is commonly applied to gravity field data of impact structures to determine the mai...
Geophysical surveys were conducted in Bukit Bunuh area, Perak to study an hypothesis of the existenc...
Forward modeling is commonly applied to gravity field data of impact structures to determine the mai...
Forward modeling is commonly applied to gravity field data of impact structures to determine the mai...
Forward modeling is commonly applied to gravity field data of impact structures to determine the mai...
Alluvial tin mining in Karangan area was closely related to the mineralization of Bongsu Granite and...
Gravity survey is one of the passive geophysical techniques commonly used to delineate geological fo...
Gravity anomalies can yield an indirect but extremely useful picture of lateral changes in rock comp...
Gravity anomalies can yield an indirect but extremely useful picture of lateral changes in rock comp...
-Geophysics investigation with the gravity method to antisipate the existence of boundary of North ...
A gravity survey was carried out in the middle of 1988 to determine the structure of the Layang-Laya...