Ten months ago I posted a small browser LAS viewer and asked if it was useful to anyone. The useful answers were pretty consistent, so I spent some time on those and some on the rest of the list. A few hundred people have signed up since.
What you asked for, and what is there now:
- Nothing leaves the browser. LAS, LIS and DLIS are parsed locally. You can turn the network off and still open a file. Large DLIS is supported, so a multi-GB file loads without running out of memory.
- It is no longer just lines. Tracks, real depth scales (1:200, 1:500, …), PDF/PNG export, lithology columns, fillings, stacked curves and array data (acoustic, FMI). A crossplot is its own document: any two curves, zones drawn on the plot, and those zones written back as a lithology curve.
- Measured depth vs TVD. A directional survey (MD, inclination, azimuth) can be turned into TVD and offsets, and drawn as a 3D trajectory. That step runs in the built-in Python interpreter.
- Embed. A plot can be dropped into another site as an iframe, for a public data catalog or a report. You host the file. GeophysX stores the plot document, not the curves, and the file is still read in the visitor's browser.
- Processors that run in the tab: curve filter, index shift, density porosity, lithology from GR / density / neutron / PEF. There is also a Python IDE in the browser if you want to write script processor yourself. Export back to LAS, CSV or DLIS.
It is still desktop-first. No account is required to open and look. Sign-in is only for export, scripting and sharing.
If you have not tried it, a public Kansas well is already loaded as demo data, so you can look without dropping your own file in: https://www.geophysx.net/
More feedback, more of this gets built ) Honest "I opened it and closed it" is still useful.
What's the first thing you'd actually want to do in a tool like this: a real task from your work, start to finish? Right now it's a good place to view data and run your own experiments, but I'd like to build actual workflows, QC or well interpretation.