Used GeoCalculator Portable for Windows?


Editors’ Review

Download.com staff
GeoCalculator performs critical structural geometrical and drillhole calculations. It handles oriented, partially oriented, and unoriented core data with flexible input/output formatting.
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GeoCalculator Portable 0/1
  • Pros

    • Performs common structural geometrical calculations
    • Supports oriented, partially oriented, and unoriented core data
    • Accepts and outputs data in varied formatting conventions
    • Converts data between different geological orientation conventions
    • Results display in numerical format and stereographic projection
  • Cons

    • Specific to geological structural data calculations
    • Method for partially oriented core is author-devised

Used GeoCalculator Portable for Windows?


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Full Specifications

GENERAL
Release
Latest update
Version
4.9.7
OPERATING SYSTEMS
Platform
Windows
Operating System
  • Windows Vista
  • Windows XP
  • Windows 7
  • Windows 10
  • Windows 2003
Additional Requirements
None
POPULARITY
Total Downloads
372
Downloads Last Week
0

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Developer’s Description

Perform common structural geometrical calculations from structural data.
GeoCalculator is based on the familiar Windows Calculator but takes geological structural data for input and output. Calculations include most common structural geometrical calculations as well as drillhole calculations for oriented, partially oriented, and unoriented core. GeoCalculator accepts and outputs structural data using a wide variety of formatting conventions for referencing lines, planes, and directions in geological space. Because input and output conventions can be set separately, GeoCalculator can be used to convert file data from one geological orientation convention and format to another. As well as a numerical results window, calculation results can be displayed in stereographic projection. Oriented drillhole calculations include not only the commonly used oriented core calculations, but also calculations for partially oriented core, a method devised by the author for using known local structural features in unoriented core as a proxy for the orientation mark in oriented core. Thus oriented core marks can be extrapolated to unoriented sections of the same core, or old unoriented core can be processed as if it were oriented.

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