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all geography including DSDP/ODP Sites and Legs
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Africa
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Namib Desert (2)
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Southern Africa
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Namibia (2)
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West Africa
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Ghana (1)
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Arctic Ocean (1)
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Arctic region
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Svalbard
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Spitsbergen (1)
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Asia
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Altai Mountains (1)
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Arabian Peninsula
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Far East
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China
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Indonesia (1)
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Korea
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Indian Peninsula
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Middle East
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Tibetan Plateau (1)
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Atlantic Ocean
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Commonwealth of Independent States
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Iberian Peninsula
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Texas (2)
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Wisconsin
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commodities
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elements, isotopes
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Invertebrata
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geochronology methods
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upper Wisconsinan
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Tertiary
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Neogene
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Miocene
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Paintbrush Tuff (1)
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Pliocene (1)
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Mesozoic
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Cretaceous
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Comanchean
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Edwards Formation (1)
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Lower Cretaceous
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Albian (1)
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Barremian (1)
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Edwards Formation (1)
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Glen Rose Formation (1)
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Mancos Shale (1)
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Upper Cretaceous
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Campanian
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lower Campanian (1)
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Ferron Sandstone Member (1)
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Frontier Formation (2)
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Lewis Shale (1)
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Maestrichtian (1)
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Turonian
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lower Turonian (1)
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Wall Creek Member (2)
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Jurassic
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Upper Jurassic
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Hanifa Formation (1)
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Navajo Sandstone (1)
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Paleozoic
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Silurian (1)
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igneous rocks
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peperite (1)
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minerals
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halides
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silicates
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sulfates
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glauberite (1)
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Primary terms
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absolute age (1)
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Africa
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Namib Desert (2)
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Southern Africa
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Namibia (2)
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West Africa
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Ghana (1)
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Arctic Ocean (1)
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Arctic region
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Svalbard
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Spitsbergen (1)
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Asia
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Altai Mountains (1)
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Arabian Peninsula
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Saudi Arabia (1)
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Far East
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China
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Zhejiang China (1)
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Indonesia (1)
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Korea
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Indian Peninsula
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Bangladesh (1)
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India
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Middle East
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Jordan (1)
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Tibetan Plateau (1)
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Atlantic Ocean
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Atlantic Ocean Islands
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Australasia
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Australia
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carbon
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Cenozoic
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middle Holocene (2)
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upper Holocene (2)
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Pleistocene
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Bishop Tuff (1)
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upper Pleistocene
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Weichselian (1)
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Wisconsinan
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upper Wisconsinan
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Fraser Glaciation (1)
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Tertiary
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Neogene
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Paintbrush Tuff (1)
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Mesozoic
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Cretaceous
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Edwards Formation (1)
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Lower Cretaceous
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Albian (1)
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Barremian (1)
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Edwards Formation (1)
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Glen Rose Formation (1)
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Mancos Shale (1)
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Upper Cretaceous
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Campanian
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lower Campanian (1)
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Ferron Sandstone Member (1)
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Frontier Formation (2)
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Lewis Shale (1)
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Maestrichtian (1)
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Turonian
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lower Turonian (1)
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Wall Creek Member (2)
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Jurassic
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Hanifa Formation (1)
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Navajo Sandstone (1)
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paleomagnetism (1)
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
dewowing
Empirical Mode Decomposition Operator for Dewowing GPR Data Available to Purchase
Dewowing of vertical radar profiling (VRP) data from Trecate. The upper row... Available to Purchase
(a) Example of the GPR profile nearest to the cliff face after dewowing. Th... Available to Purchase
Improved Hydrogeophysical Parameter Estimation from Empirical Mode Decomposition Processed Ground Penetrating Radar Data Available to Purchase
WARR data. (a) Raw data. (b) After dewow and trace normalization. Available to Purchase
GPR traces dewowed using a residual median filter. Available to Purchase
GPR traces dewowed using an empirical mode decomposition filter. Available to Purchase
Examples of vertical radar profiling (VRP) data from the Trecate site. Time... Available to Purchase
B-scans of the one-inch steel ball buried in (a) QS and (b) below the 0.015... Available to Purchase
Dewow comparison of GPR trace. The EMD and RMF results are nearly identical... Available to Purchase
Imaging Buried Culverts Using Ground Penetrating Radar: Comparing 100 MHz Through 1 GHz Antennae Available to Purchase
Abstract A 3D ground penetrating radar (GPR) survey, using three different frequency antennae, was undertaken to image buried steel culverts at the University of Houston’s La Marque Geophysical Observatory 30 miles south of Houston, Texas. The four culverts, under study, support a road crossing one of the area’s bayous. A 32 m by 4.5 m survey grid was designed on the road above the culverts and data were collected with 100 MHz, 250 MHz, and 1 GHz antennae. We used an orthogonal acquisition geometry for the three surveys. Inline sampling was from 1.0 cm to 10 cm (from 1 GHz to 100 MHz antenna) with inline and crossline spacings ranging from 0.2 m to 0.5 m. We used an initial velocity of 0.1 m/ns (from previous CMP work at the site) for the display purposes. The main objective of the study was to analyze the effect of different frequency antennae on the resultant GPR images. We are also interested in the accuracy and resolution of the various images, in addition to developing an optimal processing flow. The data were initially processed with standard steps that included gain enhancement, dewow and temporal-filtering, background suppression, and 2D migration. Various radar velocities were tried in the 2D migration and ultimately 0.12 m/ns was used. The data are complicated by multipathing from the surface and between culverts (from modeling). Some of this is ameliorated via deconvolution. The top of each of the four culverts was evident in the GPR images acquired with the 250 MHz and 100 MHz antennas. For 1 GHz, the top of the culvert was not clear due to the signal’s attenuation. The 250 MHz shielded antenna provides a vertical resolution of about 0.1 m and is the choice to image the culverts. The 100 MHz antenna provided an increment in depth of penetration, but at the expense of a substantially diminished resolution (0.25 m).