Monday, August 25, 2014

Greater Northwest Arkansas

It has taken some serious time and effort, but I can finally make GMT dance a little bit.  This map uses the NOAA ETOPO1 elevation model (1 arc-minute grid) that is a 933MB file for the entire earth surface.  Fayetteville AR (FAY) is shown as red dot, with high-elevation Boston Mountains south and East of the city. Red outline is the MArkUP study area in which we are researching Mississippian carbonates.  

Friday, August 22, 2014

Petroacoustics Book (free online)

I got this email today from Patric Rasolofosaon, whom I met at my DISC lecture in Paris. He is a world authority on poroelasticity and has a new book co-authored with Bernard Zinszner.  They have altruistically made the book free online. Chapters 1-3 (of 7) are available now

It is a rare treat when a first-class scientist writes a book synthesizing the state of knowledge and experimental evidence in any field.  On behalf of geophysicists everywhere, thank you Patrick (and Bernard)!

--------------------------------------------------------------------

Dear Colleagues,

My co-author, Bernard Zinszner,  and myself are pleased to announce the publication of our book entitled ‘Petroacoustics – A tool for Applied Seismics –‘ on the website of the eBooks of IFP Energies nouvelles
(http://books.ifpenergiesnouvelles.fr/ebooks ... Free download!).   We are very much interested in your feedback. So please do not hesitate to contact us.

By the way, please could you pass the info among your students. Indeed we are also very much interested in  Students' feedback.  Because as we wrote somewhere in the book,  the Rock Acoustics courses taught at IFP School and at the Universities Pierre et Marie Curie and Denis Diderot of Paris, and the numerous questions of the students have also greatly stimulated the writing of this book.

Thanks very much in advance for passing the information.

Best regards,

Patrick Rasolofosaon and Bernard Zinszner

---- Patrick N.J. Rasolofosaon --------
IFP Energies nouvelles
Geosciences division
Geophysics-Geomechanics Department
1 et 4 avenue de Bois Préau
92852 Rueil Malmaison - France
tel: 33(1)47.52.68.53

---------------------------------------

P Please don't print this e-mail unless you really need to.

Friday, August 15, 2014

OpendTect project portability

I have been doing many 3D seismic interpretation projects recently using OpendTect (OD). I have written elsewhere about its many wonderful features, but for the last week it was driving me nuts.

The back story is that I work across four different machines: Mac laptop, home iMac, office Mac Pro, and office windows machine.  OD data directories are on each machine, plus a common repository on my 1.5TB USB drive.  That is 5 data locations that have to be synced as interpretation goes forward.

When you start using OD, an OD data directory must be established and this holds project folders.  Within each project there are several folders to hold various kinds of information and files:


Two kinds of files are at issue in this note, session and horizon files.  First, session files (xxx.sess) live in the Misc directory and hold information to restore workspace exactly as it was when you saved the session.  Second, horizon files are stored in the Surfaces directory.  As a horizon is created, tracked and then saved, two files are created (xxx.hor and xxx.ts).

Now to the issue.  Earlier this week I was working on a small area inside a 3D seismic survey in SE Kansas.  I limited the work area, got a couple of lines open and a time slice, tracked new horizons (Miss and Woodford), then saved the session.  All this was on my laptop.  To sync my USB version of the OD data, I dropped the session file into the appropriate Misc folder and the horizon files into the Surfaces folder.

Later in the week, I was working at home and copied the new files to my OD directory on my iMac, launched OD, and opened the new session file. Or at least attempted to.  That is the rub, even though I could see the new .sess file from the Mac finder (it was there), the session load dialog box in OD did not show it.  The same thing happened with the horizons, they were there in the correct folder but OD did not see them for loading.

I suspected different operating systems (nope, all same version of OS X), different OD versions (nope, all 4.6).  I examined the new session file and compared to older ones that loaded; was there any difference in permissions or other properties? Nope.  Suspected the creation date was the issue, so manually changed it with unix command line; nope. Only the machine that created the session file could see it, ditto for surfaces. This cut right to the heart of project portability.

Diving into the Misc directory with a unix command line, I noticed an invisible .omf file.  Looking inside I saw something like this:
dTect V4.6
Object Management file
Fri 15 Aug 2014, 09:43:20
!
ID: 100070`7
!
Misc: 1
Miscellaneous directory: dGB`Stream
$Name: Misc
!
Radcliff: 2
Session setup: dGB`Stream
$Extension: sess
$Name: Radcliff.sess
#Created.At: Mon 14 Apr 2014, 18:25:14
#Created.By: Steve Milligan
!
Then it dawned on me. This is a database file that is updated when a new session or horizon is created.  By only copying the .sess or .hor/.ts files to other machines, the .omf did not get updated on that machine and therefore the new files could not be loaded.  Eureka!!

So the answer (now) is simple.  OpendTect project portability is a snap.  When you create a new horizon or session and want to port it to another machine, drag the whole Misc or Surfaces folder to the new machine and replace the old folder.  The .omf file goes along for the ride and your work will be available on the new machine.  Sweet.

Followup note: OD uses these invisible dot files as a native unix database. I find this far superior to other interpretation systems that hook into a commercial database.  In teaching my 3D seismic interpretation class, we have up to 30 students working across a network via shared drive. Database problems always arise requiring IT staff intervention, a major pain that can be completely avoided with OD. Maybe for some level of complexity a commercial database is necessary, like too many wells or surfaces or multiple users interpreting the same project. But I have not yet bumped into that limit. The chance to run an interpretation class across multiple platforms without any database is very appealing.

Thursday, August 14, 2014

Latest Ozarks Stratigraphic Column

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