Best Geology and Seismic Software for Linux of 2024

OpendTect software is made up of two parts. One is an open-source, free part, and the other is a commercial, closed source part that is protected with FlexNet license management software. OpendTect is the open-source component. It is a seismic interpretation software system that can interpret 2D and 3D seismic data. It also allows for rapid development of innovative interpretation tools. OpendTect can easily be extended by free plugins. OpendTect Pro is the closed-source version. This extended version offers additional functionality for professionals. OpendTect Pro can also be extended with plugins from the commercial sector that allow for unique seismic interpretation workflows.

SOFTWARE PLATFORM FOR ROCK+, ROCK, ALTUS AND Q330 FAMILY OF PRODUCTS Rockhound, originally introduced as SMARTS, is a software platform designed to implement real time data acquisition solutions from streams of one or more digitizers and perform vital functions on the data that are critical to the end user.The platform is modular as a building block structure where each module within specific implementation may be connected in many useful and different ways. The Rockhound software platform was developed in Java and can be used on a variety operating systems, including Microsoft Windows, multiple Mac OSs, and Linux. An optional Software Development Kit is also available that allows users create custom Rockhound modules to integrate with existing modules from Kinemetrics. The optional kit allows users to create custom post processing, data storage and notification functions.

Tecplot focus helps you get answers faster and allows you to quickly plot all of your engineering and test data exactly how you want. Analyze and analyze complex data, create multiple XY, 2D, and 3D plots, then communicate your findings to colleagues and managers with stunning, high-quality animations and images. Automating routine data analysis and plotting tasks can help you save even more time and effort. Tecplot Focus is available on Windows, Linux, and Mac platforms. It meets the needs for multi-platform engineering groups.

GeoThrust was designed with a workflow architecture in mind to produce an accurate earth model and image in time and depth from data that has been collected with irregular geometry in areas of complex topography, complex near surface, and complex subsurface. It is easy to learn and simple to use, with high technical specifications for data analysis. Nonlinear tomography is used to estimate the near-surface model. This accounts for topography and reduces vertical and lateral velocity variations. Wavefield dating is used to correct the near-surface model. This is essential for imaging from irregular topography. GeoThrust does subsurface velocity modeling, imaging, and estimation from topography. It is not based on a flat datum. Instead, it uses rms and interval speeds that are calculated at reflector positions and not at reflection positions.

The 10 largest seismic networks outside of Japan use the Antelope mission-critical data processing and data acquisition software. It is 100% commercially owned and supported entirely by BRTT, Inc., a Kinemetrics strategic partnership. You can tie-in with almost any seismic network in the World. Unique automated real-time response spectrum computation with exceedance alarms. Richly documented APIs to interface with client programs.

MiVu™, a software package, is designed to perform microseismic analysis during hydraulic fracturing. It can be used for both surface and downhole geophone arrays. MiVu™, which can be used to build simple and complex geologic models interactively and to design optimal microseismic monitoring geometries, process data with user-defined workflows and image event locations using multiple techniques. It also allows you to visualize and interpret microseismic events 3D. Multiple event location methods are available, including cross double difference, 3D grid search, 3D migrating, and 3D grid search. This allows you to see how different geophysical methods affect the location of the microseismic events. It will help you to understand the strengths and weaknesses of each method.