|
Aeromagnetic and gravity data of the Central Transantarctic Mountains Entry ID: nsf0232042 |
||||||||
|
[
Update this Record
]
|
Summary
|
Abstract:
Near complete coverage of the East Antarctic shield by ice hampers geological study of crustal architecture important for understanding global tectonic and climate history. Limited exposures in the central Transantarctic Mountains (CTAM), however, show that Archean and Proterozoic rocks of the shield as well as Neoproterozoic-lower Paleozoic sedimentary successions were involved in oblique convergence associated with Gondwana amalgamation. Subsequently, the area was overprinted by Jurassic magmatism and Cenozoic uplift. To extend the known geology of the region to ice-covered areas, we conducted an aeromagnetic survey flown in draped mode by helicopters over the Transantarctic Mountains and by fixed-wing aircraft over the adjacent polar plateau. We flew >32,000 line km covering an area of nearly 60,000 km2 at an average altitude of 600 m, with average line spacing 2.5 km over most areas and 1.25 km over basement rocks exposed in the Miller and Geologists ranges. Additional lines flown to true north, south and west extended preliminary coverage and tied with existing surveys. Gravity data was collected on the ground along a central transect of the helicopter survey area. From December 2003 to January 2004, the CTAM group flew a helicopter and twin-otter aeromagnetic survey and collected gravity station data on the ground in profile form. These data will be integrated with other geologic and geophysical data in order to extend the known geology of the region to ice-covered areas. |
| N: -82.35733 | S: -83.95234 | E: 170.21844 | W: 139.27539 |
|
Data Set Citation
|
Dataset Originator/Creator:
E. D. Anderson, C. A. Finn, D. Damaske, J. D. Abraham, F. Goldman
Dataset Title: Aeromagnetic data over the Central Transantarctica Mountains (CTAM) |
Temporal Coverage
| Start Date: 2003-12-27 |
| Stop Date: 2004-01-25 |
Location Keywords
|
CONTINENT
> ANTARCTICA
GEOGRAPHIC REGION > POLAR |
Data Resolution
|
Latitude Resolution:
625 meters
Longitude Resolution: 625 meters |
Science Keywords
| LAND SURFACE >GEOMORPHOLOGY >TECTONIC LANDFORMS/PROCESSES [Definition] |
| SOLID EARTH >GRAVITY/GRAVITATIONAL FIELD >GRAVITATIONAL FIELD [Definition] |
| SOLID EARTH >GRAVITY/GRAVITATIONAL FIELD >GRAVITY [Definition] |
| SOLID EARTH >GRAVITY/GRAVITATIONAL FIELD [Definition] |
| SOLID EARTH >GEOMAGNETISM >MAGNETIC FIELD >MAGNETIC ANOMALIES [Definition] |
| SOLID EARTH >GEOMAGNETISM >MAGNETIC FIELD [Definition] |
| SOLID EARTH >GEOMORPHIC LANDFORMS/PROCESSES >TECTONIC LANDFORMS [Definition] |
| SOLID EARTH >TECTONICS >PLATE TECTONICS >FAULT MOVEMENT [Definition] |
| SOLID EARTH >TECTONICS >PLATE TECTONICS [Definition] |
ISO Topic Category
|
GEOSCIENTIFIC INFORMATION
STRUCTURE |
Platform
| HELICOPTER [Information] |
| DHC-6 >DeHavilland Twin Otter [Information] |
Instrument
| MAGNETOMETERS [Information] |
| MAM >Magnetic Field Instrument [Information] |
Quality
|
The data in this file were collected by a single contractor (CTAM) who were responsible for collecting and processing the data. The data from this survey were collected using the same instruments (magnetometers and navigational systems) throughout the survey and were collected in a normal length of time with no long delays between survey beginning and end. Standard industry practices of the time were followed in data collection and processing. High- resolution horizontal position of the survey aircraft used to collect data were determined from GPS satellites. Positioning data were recorded in-flight independently using a Trimble 4000 and an Ashtech Surveyor 12 receivers. When possible a differential position was calculated. When not an autonomous position was used. Positions were good to one meter when differentially processed and 20 meters when autonomous was used. The cesium magnetometer is accurate to about 0.002 nanoteslas (nT) at 1 Hz and the proton precession base station magnetometer is accurate to about 1 nT. Therefore the accuracy of the base station corrected data is 1 nT or better. |
Keywords
| Aeromagnetic data |
| Central Transantarctic Mountains |
Data Set Progress
| COMPLETE |
Originating Center
Data Center
|
Mineral Resource Program, Geology Division, U.S. Geological Survey, U.S. Department of the Interior
[Information]
Data Center URL: http://minerals.usgs.gov/
| |||
Distribution
|
Distribution_Media:
electronic
Fees: none |
Personnel
|
CAROL
A
FINN Role: INVESTIGATOR Role: DIF AUTHOR Phone: 303-236-1345 Fax: 303-236-1229 Email: cfinn at usgs.gov Contact Address: U.S. Geological Survey MS 964 Denver Federal Center City: Denver Province or State: CO Postal Code: 80225 Country: USA |
Creation and Review Dates
DIF Creation Date:
2005-08-16
Last DIF Revision Date:
2008-08-29
| [ Update this Record ] |



