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snippet: The main purpose of this dataset is to provide regional-scale guidance as to the subsurface elevation of the potential units which may be suitable for deep geologic sequestration. This data should not be used as a substitute for detailed site investigations. This project was funded by the U.S. Department of Energy DE-FE0031836.
summary: The main purpose of this dataset is to provide regional-scale guidance as to the subsurface elevation of the potential units which may be suitable for deep geologic sequestration. This data should not be used as a substitute for detailed site investigations. This project was funded by the U.S. Department of Energy DE-FE0031836.
accessInformation: Midwest Regional Carbon Initiative (MRCI)
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maxScale: 50000
typeKeywords: []
description: <DIV STYLE="text-align:Left;"><DIV><DIV><P><SPAN>This is a structure contour map constructed upon the top of Pre-Mesozoic basement in the Delaware, Maryland, New Jersey, and New York coastal plain and offshore continental shelf areas. Structure contours are from Benson's 1984 map of the Baltimore Canyon Trough. Original mapped contours were in meters, digitized and converted to a grid, and extracted as a vector shapefile in contours FEET. Revisions along the Delaware, Maryland and southern New Jersey onshore coastal plain areas are from an unpublished draft map manuscript (J.W. Horton, Jr., written commun., 2022).</SPAN></P><P><SPAN>Author/Originator: Tom Sparks, Kentucky Geological Survey</SPAN></P><P><SPAN>Date Created: 2023</SPAN></P><P><SPAN>Map reference: Benson, R.N., 1984, Structure Contour Map of Pre-Mesozoic Basement, Landward Margin of Baltimore Canyon Trough: Delaware Geological Survey, University of Delaware, Miscellaneous Map Series 2, http://udspace.udel.edu/handle/19716/4288</SPAN></P></DIV></DIV></DIV>
licenseInfo: <DIV STYLE="text-align:Left;"><DIV><DIV><P STYLE="margin:0 0 11 0;"><SPAN><SPAN>This product of the Midwest Regional Carbon Initiative (MRCI) is intended to provide general geologic information only and should not be used for any other purpose. It is not intended for resale or to replace site-specific investigations. These data were compiled by MRCI, which reserves the publication rights to this material. If these data are used in the compilation of other data sets or maps for distribution or publication, this source must be referenced.</SPAN></SPAN></P><P STYLE="margin:0 0 11 0;"><SPAN><SPAN>The information contained herein may be updated or edited in the future. Future releases of this material, if altered, will display a revision date. Users should check to ensure they have the latest version and reference the appropriate revision date if it is being used in other works. </SPAN></SPAN></P><P STYLE="margin:0 0 11 0;"><SPAN>This material was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government, nor any agency thereof, nor any of their employees, nor Battelle, nor any member of the MRCI makes any warranty, express or implied, or assumes any liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendations, or favoring by Battelle, members of the MRCI, the United States Government or any agency thereof. The views and the opinions of authors expressed herein do not necessarily state or reflect those of the members of the MRCI, the United States Government or any agency thereof.</SPAN></P></DIV></DIV></DIV>
catalogPath:
title: Subsurface Structure Contours on the top of the Pre-Mesozoic basement of the MRCI region
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tags: ["CCUS","MRCI","Structure Contours","Basement","Pre-Mesozoic","Delaware","Maryland","New Jersey","New York","coastal plain","offshore","continental shelf","Baltimore Canyon Trough"]
culture: en-US
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minScale: 20000000
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