Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Bulletin of Canadian Petroleum Geology Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Bulletin of Canadian Petroleum Geology; September 2006; v. 54; no. 3; p. 221-237; DOI: 10.2113/gscpgbull.54.3.221
© 2006 Canadian Society of Petroleum Geologists
This Article
Right arrow Résumé
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Submit a response
Right arrow Alert me when this article is cited
Right arrow Alert me when eLetters are posted
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Web of Science (1)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Gentzis, T.
Right arrow Articles by Santillan, M.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Horizontal degasification and characterization of coals in the Sabinas Sub-basin, Mexico: implications for CBM production

Thomas Gentzis, Keith Murray, Renee Klinger and Mario Santillan

Formerly with CDX Gas, LLC Suite 1060, 1801 Broadway Denver, CO 80202, USA
CDX Gas, LLC Suite 190, 5485 Beltline Road Dallas, TX 75254, USA
Minerales Monclova S.A. de C.V., Prol. Pdte. Cardenas S/N, Apartado Postal No. 47, C.P. 26350, Palau, Coahuila, Mexico
CDX Canada, Co. Suite 1210, 606 - 4th Street SW Calgary, AB T2P 1T1, Canada

The Sabinas sub-basin in northern Mexico contains gassy coals in the Upper Cretaceous Los Olmos Formation, based on both historical evidence and current desorption testing. The "Double Seam" coal is present at shallow depth (<500 m), has high vitrinite content (>86 vol%), is well-cleated, shows high diffusivity [average tau ({tau}) value is 56 hours] and has high natural fracture permeability (>30 mD) in the minesites. The coal averages 2.2 m in thickness but has a high ash content (32 wt%). A tonstein band is present in the middle of the Double Seam, consisting of vitrinite and inertinite embedded in a matrix of fine clays and quartz. Average desorbed gas content of this medium-volatile bituminous coal 3/g). Maximum methane adsorption at an equivalent (Romax = 1.30%) is highest in Mine V (Esmeralda Mine at >9.0 cm depth of 300 m is 15 cm3/g (as-received basis; arb). Coal bed methane is mainly methane (98%) with heating value of 38.21 MJ/m3 (1026 Btu/ft3). The coal is under-pressured and reported to be dry, with possibly free gas in the cleat/fracture system and absence of discrete mineralization. In-seam horizontal drilling prior to longwall mining has resulted in the significant reduction of in-situ gas contents and in an increase of mined coal production per shift. The Sabinas sub-basin coals are suitable for a full-scale coal bed methane (CBM) development using in-seam single horizontal and multi-lateral horizontal drilling. Similarities, but also differences, exist between the Sabinas coals in Mexico and the same coals in the Maverick Basin, Texas.







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Canadian Society of Petroleum Geologists