Transcript Using aeromagnetics to explore for Trenton
Interim Report of the West-Central New York Lineament Consortium
Dr. Robert Jacobi University at Buffalo Joseph P. Fagan, Jr.
Centennial Geoscience, Inc.
Acknowledgements
• This work was contracted for, and sponsored by, the New York State Energy Research and Development Authority (NYSERDA).
• Pennsylvania aeromagnetic data courtesy of AGI.
Objectives
• Describe the thinking behind the West Central New York Lineament Consortium • Review work to date and future plans • Discuss how to participate
Background
• Present day topography reveals many clues about the subsurface geology.
• Work at SUNY has demonstrated the concept of fracture intensification domains, or FIDs.
• How do these FIDs compare information on topographic maps?
with
#8
. ENE-STRIKING FID
Background
• Aeromagnetic data provide information about faulting patterns in the basement.
• As basement is brittle, lithologic contacts also can become the loci for fracturing.
• Reactivated basement faults can propagate fractures upwards through the sedimentary column.
SENECA LAKE TRANSECT ENE VALOIS HECTOR EW ENE EW FRACTURES LINEAMENTS 2.5
1.5
0.5
0 15 SOIL GAS 10 5 0 SOUTH 32 28 24 20 16 12 8 4 0 NORTH U B
Rock Fracture Group
2 km
“Sandwiching” the fractures
• By combining the two methods—top down and bottom up—can we find areas of coincidental fracturing and/or faulting?
• If so, could these two sets be part of one continuous system that extends up from the basement and all the way to surface?
Study area
• Study area covers an area of western New York about 5,200 square miles • 98 7-1/2’ quadrangles in study area • Part of, or all of, thirteen counties within area
Map of study area
Data sets used in study
• High-resolution aeromagnetic data set flown by Geologic Survey of Canada in 1999 • Newest version of digital elevation models (DEM) from USGS—data points every ten meters on orthogonal grid • Earthsat 1997 study
Outline of work
• DEM Compilation and Mapping • Aeromagnetic/gravity processing • Geophysical and Remote Sensing Integration • Final integration and analysis
DEM Compilation
• 98 7-1/2’ quads were gridded and mapped.
• These grids were individually analyzed, and also merged into 15’ x 15’ quadrangles to permit easier analysis.
• Curvature analyses were run to identify possible FIDs.
Curvature?
• Curvature is a 2-D property that describes how bent a curve is at a particular point.
• Curvature depends on the scale that it is examined at.
• Areas of high curvature (topographically) occur on slope breaks such as hillsides and stream edges.
Outline of work
• DEM Compilation and Mapping • Aeromagnetic/gravity processing • Geophysical and Remote Sensing Integration • Final integration and analysis
Aeromagnetic/gravity work
• Reprocess and interpret existing high resolution aeromagnetic data • Reprocess and interpret existing gravity data • Integrate to complete structural interpretation
Outline of work
• DEM Compilation and Mapping • Aeromagnetic/gravity processing • Geophysical and Remote Sensing Integration • Final integration and analysis
Geophysical / Remote Sensing Integration
• Merge DEM attributes with Earthsat’s Landsat lineaments.
• Compare these with structural interpretation from previous step to determine a subset of lineaments that may be related to basement structures.
Lineaments from EarthSat, 1997 50 mi 50 km -
Lineaments from EarthSat, 1997 50 mi 50 km -
Outline of work
• DEM Compilation and Mapping • Aeromagnetic/gravity processing • Geophysical and Remote Sensing Integration • Final integration and analysis
Final Analysis
• Determine which major lineaments are most likely to be related to basement faulting.
• Create integrated map showing areas of faulting/fracturing at both basement and surface levels.
Participating in the consortium
• Anyone may participate—private industry, government organization, or university.
• Consortium members will receive: DEM data and derivatives, aeromagnetic data w/ interpretation, gravity data, integrated maps showing areas of faulting/fracturing at both basement and surface levels, and summary reports.
Participating in the consortium
• Purchase price to participate: $5,000 for the entire area.
• Anticipated completion date: Spring, 2005.