Gravity gradient anomaly map. Contour interval at 5 µGal/m with bolder
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![](https://www.researchgate.net/publication/233308007/figure/fig3/AS:373710226771973@1466110869739/Gravity-gradient-anomaly-map-Contour-interval-at-5-Gal-m-with-bolder-lines-at-20-Gal-m.png)
![](https://static.cambridge.org/binary/version/id/urn:cambridge.org:id:binary-alt:20210916180333-44944-mediumThumb-84288fig4_19.jpg?pub-status=live)
Gravity and Magnetics (Chapter 4) - Integration of Geophysical Technologies in the Petroleum Industry
![](https://se.copernicus.org/articles/10/599/2019/se-10-599-2019-f03.png)
SE - Time-lapse gravity and levelling surveys reveal mass loss and ongoing subsidence in the urban subrosion-prone area of Bad Frankenhausen, Germany
![](https://media.cheggcdn.com/media/8b9/8b943f51-d79d-4d64-a827-583b9613d8c6/phpeJiahC.png)
The figure below shows a map of the Bouguer gravity
![](https://www.researchgate.net/profile/Fabio-Caratori-Tontini/publication/233308007/figure/fig4/AS:373710226771977@1466110870233/a-b-Gradient-signal-up-and-depth-of-gravel-layer-down-along-the-two-arms-of-the_Q320.jpg)
Gravity gradient anomaly map. Contour interval at 5 µGal/m with bolder
![](https://www.researchgate.net/profile/Jan-Svancara-2/publication/226018900/figure/fig3/AS:393823344709663@1470906210832/Bouguer-anomaly-contour-map-The-contour-interval-is-2-mGal-20-pim-s2-Gravity_Q320.jpg)
Bouguer anomaly contour map. The contour interval is 2 mGal = 20
![](https://agupubs.onlinelibrary.wiley.com/cms/asset/22799036-aec7-4422-b19b-0a49dc849809/grl52009-fig-0002-m.jpg)
Antarctic outlet glacier mass change resolved at basin scale from satellite gravity gradiometry - Bouman - 2014 - Geophysical Research Letters - Wiley Online Library
![](https://static.cambridge.org/binary/version/id/urn:cambridge.org:id:binary:20190405080315572-0607:9781316480724:13749fig7_7.png?pub-status=live)
Geophysical Techniques (Part II) - Geophysics and Geosequestration
![](https://d3i71xaburhd42.cloudfront.net/e2ff70e975c1268c3038b0cf960f089ccb0951df/5-Figure4-1.png)
PDF] Normalized Full Gradient of Gravity Anomaly Method and Its Application to the Mobrun Sulfide Body, Canada
![](https://www.researchgate.net/profile/Animesh-Mandal-3/publication/235933237/figure/fig4/AS:670034963742746@1536760192973/Residual-gravity-anomaly-map-with-contour-interval-of-06-mGal-AA-and-BB-are-the-two_Q320.jpg)
Residual gravity anomaly map with contour interval of 0.6 mGal. AA′ and
![](https://essd.copernicus.org/articles/13/2165/2021/essd-13-2165-2021-f17-high-res.png)
ESSD - The first pan-Alpine surface-gravity database, a modern compilation that crosses frontiers
![](https://www.researchgate.net/profile/Hernan-Ugalde-2/publication/228493879/figure/fig5/AS:302042494062598@1449023950734/Bathymetry-of-Lake-Wanapitei-The-greatest-depths-of-approximately-120-m-are-found-in-the_Q320.jpg)
PDF) Measuring gravity on ice: An example from Wanapitei Lake, Ontario, Canada
![](https://i1.rgstatic.net/ii/profile.image/332298600894464-1456237568096_Q64/Soumen-Koley.jpg)
PDF) Microgravity vertical gradient measurement in the site of
![](https://c5.rgstatic.net/m/4671872220764/images/template/default/profile/profile_default_m.jpg)
PDF) Microgravity vertical gradient measurement in the site of
![](https://www.frontiersin.org/files/Articles/1068435/feart-10-1068435-HTML/image_m/feart-10-1068435-g007.jpg)
Frontiers Analysis of the coseismic slip behavior for the MW = 9.1 2011 Tohoku-Oki earthquake from satellite GOCE vertical gravity gradient
![](https://www.researchgate.net/publication/285236494/figure/fig1/AS:614003072049154@1523401148113/Gravity-anomaly-map-with-an-assumed-density-of-2300-kg-m-3-Contour-interval-is-05-mgal.png)
Gravity anomaly map with an assumed density of 2300 kg/m 3. Contour
1. As an exploration geologist working for an oil
3. As an exploration geologist working for an oil
Regional gravity anomaly map with contour interval of 0.1 mGal.
The gravity disturbance contour map of study area
A) shows an elevation contour map created using gravity data. The
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