DOCSLIB.ORG

Pre-San Andres Stratigraphy and Oil-Producing Zones in Southeastern New Mexico a PROGRESS REPORT

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Pre-San Andres Stratigraphy and Oil-Producing Zones in Southeastern New Mexico a PROGRESS REPORT NEW MEXICO BUREAU OF MINES AND MINERAL RESOURCES A DEPARTMENT OF THE SCHOOL OF MINES E. C. ANDERSON Director BULLETIN 29 Pre-San Andres Stratigraphy and Oil-Producing Zones in Southeastern New Mexico A PROGRESS REPORT By E. RUSSELL LLOYD SOCORRO 1949 CONTENTSP Page The New Mexico Bureau of Mines and Mineral Resources ------------------------ 6 Board of Regents ------------------------------------------------------------------ 6 Explanatory note ------------------------------------------------------------------------ 7 Introduction ----------------------------------------------------------------------------- 9 Acknowledgments --------------------------------------------------------------------- 10 Principal structural features --------------------------------------------------------- 11 General 11 Pedernal Mountains -------------------------------------------------------------- 13 Matador uplift -------------------------------------------------------------------- 15 Eunice uplift ---------------------------------------------------------------------- 15 Stratigraphy ---------------------------------------------------------------------------- 17 General outline 17 Permian system ------------------------------------------------------------------- 18 Classification 18 Guadalupe-Leonard contact ----------------------------------------------- 19 Guadalupe or Leonard series --------------------------------------------- 22 Glorieta sandstone ---------------------------------------------------- 22 Leonard series --------------------------------------------------------------- 23 Yeso formation --------------------------------------------------------- 23 Victorio Peak reef zone 27 Leonard and Wolfcamp ( ?) series ---------------------------------------- 28 Abo formation ---------------------------------------------------------- 28 Wolfcamp series ------------------------------------------------------------- 31 Hueco limestone 31 Bursum formation ---------------------------------------------------- 32 Hueco and Bursum formations in subsurface -------------------- 33 Pennsylvanian system ----------------------------------------------------------- 34 General features ------------------------------------------------------------ 34 Virgil series ------------------------------------------------------------------ 37 Missouri series 38 Des Moines series ----------------------------------------------------------- 39 Atoka series ----------------------------------------------------------------- 40 Mississippian system ------------------------------------------------------------ 40 General features 40 Chester series --------------------------------------------------------------- 42 Helms formation ------------------------------------------------------ 42 Meramec series -------------------------------------------------------------- 44 Rancheria formation -------------------------------------------------- 44 Osage series ----------------------------------------------------------------- 45 Lake Valley formation ------------------------------------------------- 45 Kinderhook series ----------------------------------------------------------- 45 Caballero formation -------------------------------------------------- 45 Devohian system ----------------------------------------------------------------- 46 General features 46 3 4 CONTENTS Page Upper Devonian 48 Woodford formation -------------------------------------------------- 48 Percha shale 48 Contadero and Sly Gap formations 49 Middle Devonian------------------------------------------------------------- 49 Oñate formation ------------------------------------------------------- 49 Canutillo formation --------------------------------------------------- 50 Lower Devonian ------------------------------------------------------------- 51 Silurian system ------------------------------------------------------------------- 52 Ordovician system --------------------------------------------------------------- 54 Upper Ordovician ----------------------------------------------------------- 54 Montoya formation ---------------------------------------------------- 54 Middle Ordovician ---------------------------------------------------------- 56 Simpson group -------------------------------------------------------- 56 Lower Ordovician 57 Ellenburger group and El Paso limestone ------------------------- 57 Cambrian system ---------------------------------------------------------------- 59 Geological history 59 Cambrian -------------------------------------------------------------------------- 59 Ordovician 59 Silurian ---------------------------------------------------------------------------- 60 Devonian 61 Mississippian --------------------------------------------------------------------- 61 Pennsylvanian 62 Permian ---------------------------------------------------------------------------- 63 Oil and gas pools 64 General ---------------------------------------------------------------------------- 64 Permian pools of the Leonard and Wolf camp series ------------------------ 67 Pennsylvanian pool 67 Mississippian pool --------------------------------------------------------------- 68 Devonian pool --------------------------------------------------------------------- 68 Silurian pools --------------------------------------------------------------------- 68 Ordovician pools ----------------------------------------------------------------- 69 Future possibilities for pre-San Andres production ------------------------------- 69 Selected bibliography ------------------------------------------------------------------ 73 Index -------------------------------------------------------------------------------------- 77 Publications of the New Mexico Bureau of Mines and Mineral Resources 81 PLATES Facing • Page 1. Pre-San Andres oil and gas map of southeastern New Mexico In pocket 2. Comparative sections of Permian formations: Surface sections -------------------------------------------------------- In pocket 3. Comparative sections of Yeso formation in selected wells In pocket 4. Comparative sections of Pennsylvanian system: Surface and subsurface ----------------------------------------------- In pocket 5. Outline cross section: Guadalupe County to eastern Lea County ----------------------------------------------------------------------- 22 6. Outline cross section: Chaves County to eastern Lea County 30 7. Outline cross section: Southwestern Chaves County to northern Lea County ----------------------------------------------------------- 32 8. Outline cross section; south to north: eastern Lea County 42 9. Outline cross section ; west to east: Eunice area 56 10. Composite stratigraphic section, Lea County --------------------------- 64 FIGURES Page 1. Index map ---------------------------------------------------------------------- 8 2. Pre-Cambrian elevations in southeastern New Mexico ----------------- 12 3. Correlation chart, Permian formations in New Mexico ----------------- 16 4. Pennsylvanian system in southeastern New Mexico ------------------- 36 5. Mississippian system in southeastern New Mexico -------------------- 43 6. Devonian and Silurian systems in southeastern New Mexico 47 7. Ordovician system in southeastern New Mexico ------------------------ 55 THE NEW MEXICO BUREAU OF MINES AND MINERAL RESOURCES The New Mexico Bureau of Mines and Mineral Resources, designated as "a department of the New Mexico School of Mines and under the direction of its Board of Regents," was established by the New Mexico Legislature of 1927. Its chief functions are to compile and distribute information regarding mineral industries in the State, through field studies and collections, laboratory and library research, and the publication of the results of such investigations. A full list of the publications of the New Mexico Bureau of Mines and Mineral Resources is given on the last pages of this Bulletin. BOARD OF REGENTS HIS EXCELLENCY, HONORABLE THOMAS J. MABRY, Governor of New Mexico, ex-officio ----------------------------------------------------------------- Santa Fe CHARLES L. ROSE, Superintendent of Public Instruction, ex-officio ---------------------------------------------------------------------------------------- Santa Fe J. H. RUSSELL, President --------------------------------------------------------------------- Santa Fe T. M. CRAMER, Secretary and Treasurer ---------------------------------------------- Carlsbad T. E. DABNEY --------------------------------------------------------------------- Socorro COOPER SHAPLEY -------------------------------------------------------------- Deming G. T. HARLEY ------------------------------------------------------------------ Carlsbad EXPLANATORY NOTE By E. C. ANDERSON The four years since the release of Bulletin No. 23, a preliminary report compiled by Robert E. King, have seen much work done and great progress made in the search for oil at depth in southeastern New Mexico. Many wells have been drilled, many producers have been brought in, and several new fields developed. Much new information on the stratigraphy and producing zones of the pre-San Andres formations has been accumulated. The Bureau deemed it desirable that a new report be compiled and published that would include all the information, new and old, available as of July 1, 1949—that a "Progress Report" be made to replace Mr. King's "Preliminary Report". To do the job properly it was essential that a person familiar with what has been done in the area be persuaded to undertake the work. It was not only essential that
Load more

Recommended publications
  • Map 3.1 Travel Management Plan
    TOADLENA SHEEP SPRINGS GREAT BENDTHE PILLAR 3 NW THE PILLAR 3 NE TANNER LAKE PRETTY ROCKPUEBLO BONITO NW B836108 B636108 B536108 B436108 KIMBETO LYBROOK NW LYBROOK COUNSELORTANCOSA WINDMILL B336108 B236108 B136108 FIVE LAKES CANYON NEREGINA GALLINA ARROYA DEL AGUAYOUNGSVILLE CANONES ABIQUIU Y 134 B836107 B736107 B636107 B536107 B436107 MEDANALES LYDEN VELARDE TRAMPAS PENASCO TRES RITOS CERRO VISTA CHACON W B336107 B136107 B836106 B736106 B636106 B536106 E H B436106 B336106 B236106 B136106 B836105 B736105 B636105 B536105 B436105 B336105 T TOADLENA FIVE LAKES CANYON NW U STA 8 S 6 SONSELA BUTTES B236107 CRYSTAL WASHINGTON PASS S H Y A136109 NASCHITTI CHACO CANYON T W W A836108 THE PILLAR 3 SW A H A736108 THE PILLAR 3 SE Y E A636108 LA VIDA MISSION T T E A436108 PUEBLO BONITO HW 8 A A336108 FIRE ROCK WELL Y 44 ABIQUIU 4 TAOS GREY HILL SPRING T A236108 A836107 LYBROOK SE MULE DAM DEER MESA A636107 TAYLOR RANCH CUBA S A536108 KIN KLIZHIN RUINS A536107 A436107 A336107 NACIMIENTO PEAK JAROSA POLVADERA PEAK SARGENT RANCH A236107 A836106 VALLECITOS CHILI SAN JUAN PUEBLO CHIMAYO TRUCHAS EL VALLE JICARITA PEAK HOLMAN A136108 A736106 A636106 A436106 COMANCHE PEAK A736107 ARROYO CHIJUILLITA A336106 A236106 A136106 A836105 A736105 A636105 A536105 A436105 S A336105 CERRO DEL GRANT 6 A136107 7 T A536106 Y A W T STATE H HWY STAT E E BUELL PARK TODILTO PARK 1 H CHUSKA PEAK 26 W H135109 H835108 EAR ROCK Y H735108 RED LAKE WELL 5 H535108 MILK LAKE NOSE ROCK 18 COYOTE CANYON NW H335108 SEVEN LAKES NEPUEBLO PINTADO STANDING ROCK NW H235108 H135108 STAR LAKE
    [Show full text]
  • Prepared by the U.S. Geological Survey in Cooperation with Fort
    United States Department of the Interior Geological Survey Albuquerque, New Mexico Site study for a water well, Fort Wingate Army Ordnance Depot, McKinley County, New Mexico John W. Shomaker 1* Prepared by the U.S. Geological Survey in cooperation with Fort Wingate Army Ordnance Depot Open-file report April 1968 Contents Page — 4 Introduction — The stratigraphlc section in the Fort Wingate area Consideration of aquifers for a dependable water supply 17 _________ 22 Suggested well location y 25 Production well construction 27 Sutanary ~~ References cited Illustrations Reference page Figure l.-Map showing location of Fort Wingate Army Depot, and area of well-site investigation 4 2.—Altitude of the top of Glorleta Sandstone in Tidnlty of Headquarters area — ' (In"ocket) 3.—Depth to top of Precambrian granite and depth to top of Glorieta Sandstone in vicinity of Headquarters area — (I2 ■■• •■■ Site study for * water well, Fort Wlngate Army Ordnance Depot, McKinley County, New Mexico By John W. Shomaker Introduction Th« Fort Wingate Army Depot (fig. 1) is now supplied with water r . Figure 1 (caption on next page) belongs near here. from only one source, well No. 68 which is 1,125 feet deep. The well casing is deteriorating and the well nay fail. The Depot considers this an emergency situation that requires a new well to be drilled as soon as possible. In addition, the Army Materiel Command has suggested to the Depot that the total ground-water resources of the Depot area be evaluated as an aid to long-range planning. The Depot requested the U.S. Geological Survey to suggest study plans to accomplish an evaluation of the ground-water resources.
    [Show full text]
  • GEOLOGY and GROUND-WATER SUPPLIES of the FORT WINGATE INDIAN SCHOOL AREA, Mckinley COUNTY, NEW MEXICO
    GEOLOGICAL SURVEY CIRCULAR 360 GEOLOGY AND GROUND-WATER SUPPLIES OF THE FORT WINGATE INDIAN SCHOOL AREA, McKINLEY COUNTY, NEW MEXICO PROPERTY OT§ tJ. B. EED! DGJCAL' SURVEY PUBLIC INQUIRIES OFFICE BAN FRANC1ECQ. CALIFORNIA Prepared in cooperation with the Bureau of Indian Affairs UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director GEOLOGICAL SURVEY CIRCULAR 360 GEOLOGY AND GROUND-WATER SUPPLIES OF THE FORT WINGATE INDIAN SCHOOL AREA, McKINLEY COUNTY, NEW MEXICO By J. T. Callahan and R. L. Cushman Prepared in cooperation with the Bureau of Indian Affairs Washington, D. C-, 1905 Free on application to the Geological Survey, Washington 25, D. C. GEOLOGY AND GROUND-WATER SUPPLIES OF THE FORT WINGATE INDIAN SCHOOL AREA, McKINLEY COUNTY, NEW MEXICO By J. T. Callahan and R. L. Cushman CONTENTS Page Page Abstract.................................................... 1 Geology and ground-water resources--Continued Introduction............................................... 2 Geologic structures--Continued Location, topography, and drainage............... 2 Faults..,................................................. 5 Geology and ground-water resources.............. 2 Ground water................................................ 5 Geologic formations and their water-bearing San Andres formation.................................. 5 properties........................................ 2 Recharge conditions................................. 5 Permian system................................... 4 Discharge
    [Show full text]
  • (Foram in Ifers, Algae) and Stratigraphy, Carboniferous
    MicropaIeontoIogicaI Zonation (Foramin ifers, Algae) and Stratigraphy, Carboniferous Peratrovich Formation, Southeastern Alaska By BERNARD L. MAMET, SYLVIE PINARD, and AUGUSTUS K. ARMSTRONG U.S. GEOLOGICAL SURVEY BULLETIN 2031 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Robert M. Hirsch, Acting Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Text and illustrations edited by Mary Lou Callas Line drawings prepared by B.L. Mamet and Stephen Scott Layout and design by Lisa Baserga UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1993 For sale by Book and Open-File Report Sales U.S. Geological Survey Federal Center, Box 25286 Denver, CO 80225 Library of Congress Cataloging in Publication Data Mamet, Bernard L. Micropaleontological zonation (foraminifers, algae) and stratigraphy, Carboniferous Peratrovich Formation, southeastern Alaska / by Bernard L. Mamet, Sylvie Pinard, and Augustus K. Armstrong. p. cm.-(U.S. Geological Survey bulletin ; 2031) Includes bibtiographical references. 1. Geology, Stratigraphic-Carboniferous. 2. Geology-Alaska-Prince of Wales Island. 3. Foraminifera, Fossil-Alaska-Prince of Wales Island. 4. Algae, Fossil-Alaska-Prince of Wales Island. 5. Paleontology- Carboniferous. 6. Paleontology-Alaska-Prince of Wales Island. I. Pinard, Sylvie. II. Armstrong, Augustus K. Ill. Title. IV. Series. QE75.B9 no. 2031 [QE671I 557.3 s--dc20 [551.7'5'097982] 92-32905 CIP CONTENTS Abstract
    [Show full text]
  • The Mississippian Barnett Formation: a Source-Rock, Seal, and Reservoir Produced by Early Carboniferous Flooding of the Texas C
    THE MISSISSIPPIAN BARNETT FORMATION: A SOURCE-ROCK, SEAL, AND RESERVOIR PRODUCED BY EARLY CARBONIFEROUS FLOODING OF THE TEXAS CRATON Stephen C. Ruppel and Jeffery Kane Bureau of Economic Geology Jackson School of Geosciences The University of Texas at Austin Austin,. TX ABSTRACT The Early Carboniferous (Mississippian) was a time of crustal downwarping and flooding of southern Texas region. Mississippian facies documenting this flooding include a basal, updip, shallow to deep water carbonate succession and an overlying, downdip, deep water, fine grained siliciclastic mudrock succession. The basal carbonate succession, termed the Mississippian Limestone in the Permian Basin, includes the Chappel of the Llano Uplift and the Caballero-Lake Valley of southern New Mexico outcrops. These rocks document the margins of an extensive carbonate platform that occupied much of the western U.S. during the middle developed Mississippian. The overlying siliciclastic mudrock succession includes the Barnett formation of the Permian and Ft. Worth Basins and the Rancheria Formation of southern New Mexico outcrops. These rocks accumulated by autochthonous hemipelagic sedimentation and allochthonous mass gravity transport in low energy, below wave base, dysaerobic conditions in a platform marginal deep water basin formed on the southern margin of the Laurussian platform. The carbonate section is poorly known and only of minor importance as a hydrocarbon reservoir in the Permian Basin. Key insights into the detailed character and architecture of these rocks are provided by analogous outcrops of the Lake Valley outcrop succession in New Mexico. The overlying Barnett mudrock succession, long recognized as a hydrocarbon source rock, is similarly poorly known but has recently attracted great attention as a target for gas exploration and development.
    [Show full text]
  • Stratigraphic Correlation Chart for Western Colorado and Northwestern New Mexico
    New Mexico Geological Society Guidebook, 32nd Field Conference, Western Slope Colorado, 1981 75 STRATIGRAPHIC CORRELATION CHART FOR WESTERN COLORADO AND NORTHWESTERN NEW MEXICO M. E. MacLACHLAN U.S. Geological Survey Denver, Colorado 80225 INTRODUCTION De Chelly Sandstone (or De Chelly Sandstone Member of the The stratigraphic nomenclature applied in various parts of west- Cutler Formation) of the west side of the basin is thought to ern Colorado, northwestern New Mexico, and a small part of east- correlate with the Glorieta Sandstone of the south side of the central Utah is summarized in the accompanying chart (fig. 1). The basin. locations of the areas, indicated by letters, are shown on the index map (fig. 2). Sources of information used in compiling the chart are Cols. B.-C. shown by numbers in brackets beneath the headings for the col- Age determinations on the Hinsdale Formation in parts of the umns. The numbers are keyed to references in an accompanying volcanic field range from 4.7 to 23.4 m.y. on basalts and 4.8 to list. Ages where known are shown by numbers in parentheses in 22.4 m.y. on rhyolites (Lipman, 1975, p. 6, p. 90-100). millions of years after the rock name or in parentheses on the line The early intermediate-composition volcanics and related rocks separating two chronostratigraphic units. include several named units of limited areal extent, but of simi- No Quaternary rocks nor small igneous bodies, such as dikes, lar age and petrology—the West Elk Breccia at Powderhorn; the have been included on this chart.
    [Show full text]
  • Permian Basin, West Texas and Southeastern New Mexico
    Report of Investigations No. 201 Stratigraphic Analysis of the Upper Devonian Woodford Formation, Permian Basin, West Texas and Southeastern New Mexico John B. Comer* *Current address Indiana Geological Survey Bloomington, Indiana 47405 1991 Bureau of Economic Geology • W. L. Fisher, Director The University of Texas at Austin • Austin, Texas 78713-7508 Contents Abstract ..............................................................................................................................1 Introduction ..................................................................................................................... 1 Methods .............................................................................................................................3 Stratigraphy .....................................................................................................................5 Nomenclature ...................................................................................................................5 Age and Correlation ........................................................................................................6 Previous Work .................................................................................................................6 Western Outcrop Belt ......................................................................................................6 Central Texas ...................................................................................................................7 Northeastern Oklahoma
    [Show full text]
  • West Texas Geological Society Publications and Contents Purchase from West Texas Geological Society
    West Texas Geological Society Publications and Contents Purchase from West Texas Geological Society: http://www.wtgs.org/ 77-68 Geology of the Sacramento Mountains Otero County, New Mexico Regional Distribution of Phylloid Algal Mounds in Late Pennsylvanian and Wolfcampian Strata of Southern New Mexico James Lee Wilson Growth History of a Late Pennsylvanian Phylloid Algal Organic Buildup, Northern Sacramento Mains, New Mexico D.F. Toomey, J.L. Wilson, R. Rezak Paleoecological Evidence on the Origin of the Dry Canyon Pennsylvanian Bioherms James M. Parks Biohermal Submarine Cements, Laborcita Formation (Permian), Northern Sacramento Mountains, New Mexico John M. Cys and S.J. Mazzullo Carbonate and Siliciclastic Facies of the Gobbler Formation John C. Van Wagoner The Rancheria Formation: Mississippian Intracratonic Basinal Limestones Donald A. Yurewicz Stratigraphic and Structural Features of the Sacramento Mountain Escarpment, New Mexico Lloyd C. Pray Conglomeratic Lithofacies of the Laborcita and Abo Formations ( Wolfcampian), North Central Sacramento Mountains: Sedimentology and Tectonic Importance David J. Delgado Paleocaliche Textures from Wolfcampian Strata of the Sacramento Mountains, New Mexico David J. Delgado Introduction to Road Logs Lloyd C. Pray Alamogordo to Alamo Canyon and the Western Sacramento Mountains Escarpment Field Guide and Road Log “A” Lloyd C. Pray Supplemental Field Guide to Southernmost Sacramento Mountains Escarpment – Agua Chiquita and Nigger Ed Canyons Lloyd C. Pray Alamogordo to Indian Wells Reentrant Field Guide and Road Log “B” Lloyd C. Pray Guide Locality B-1-West End of Horse Ridge John C. Van Wagoner 1 Field Guide and Road Log “C” Lloyd C. Pray Plate Shaped Calcareous Algae in Late Paleozoic Rocks of Midcontinent (abstract): James M.
    [Show full text]
  • Silver and Gold Occurrences in New Mexico by Robert M
    New Mexico Bureau of Mines & Mineral Resources Resource Map 15 March 1986 Silver and gold occurrences in New Mexico by Robert M. North and Virginia T. Mclemore New Mexico Bureau of Mines and Mineral Resources, Socorro, New Mexico 87801 Abstract Anomalous amounts of silver and/or gold have been identified in 153 mining districts or prospect areas of New Mexico. Production from most of these occurrences has been small; figures or estimates are given when known. Thirty-five districts have produced in excess of 10,000 troy ounces of gold or 200,000 ounces of silver. Silver and gold in New Mexico occur in 14 distinct types of deposits ranging in age from Precam­ brian (Proterozoic) to Recent. Mid-Tertiary to Recent deposits include the placer, volcanic-epithermal, supergene copper-uranium (silver), and Great Plains Margin types. Late Cretaceous to mid-Tertiary deposits include the sedimentary-hydrothermal barite-fluorite-galena, carbonate-hosted silver (lead­ manganese ), lead-zinc and copper skarn, Laramide vein, and prophyry-copper types. Late Paleozoic to early Mesozoic deposits include the sedimentary-copper type and possibly some of the Permian Mississippi Valley type. Precambrian deposits include the vein and replacement and Precambrian massive-sulfide types. Deposits that have produced significant silver and/or gold as the primary product are the placer, volcanic-epithermal, Great Plains Margin, carbonate-hosted silver, and Lar­ amide vein types. Deposits that have produced significant precious metals as a byproduct of base­ metal mining include the carbonate-hosted lead-zinc, copper skarn, and porphyry-copper types. Introduction Precious metals in varying degrees of importance or 14 ppm (0.41 oz/ton) silver.
    [Show full text]
  • Subsurface Geologic Plates of Eastern Arizona and Western New Mexico
    Implications of Live Oil Shows in an Eastern Arizona Geothermal Test (1 Alpine-Federal) by Steven L. Rauzi Oil and Gas Program Administrator Arizona Geological Survey Open-File Report 94-1 Version 2.0 June, 2009 Arizona Geological Survey 416 W. Congress St., #100, Tucson, Arizona 85701 INTRODUCTION The 1 Alpine-Federal geothermal test, at an elevation of 8,556 feet in eastern Arizona, was drilled by the Arizona Department of Commerce and U.S. Department of Energy to obtain information about the hot-dry-rock potential of Precambrian rocks in the Alpine-Nutrioso area, a region of extensive basaltic volcanism in southern Apache County. The hole reached total depth of 4,505 feet in August 1993. Temperature measurements were taken through October 1993 when final temperature, gamma ray, and neutron logs were run. The Alpine-Federal hole is located just east of U.S. Highway 180/191 (old 180/666) at the divide between Alpine and Nutrioso, in sec. 23, T. 6 N., R. 30 E., in the Apache-Sitgreaves National Forest (Fig. 1). The town of Alpine is about 6 miles south of the wellsite and the Arizona-New Mexico state line is about 6 miles east. The basaltic Springerville volcanic field is just north of the wellsite (Crumpler, L.S., Aubele, J.C., and Condit, C.D., 1994). Although volcanic rocks of middle Miocene to Oligocene age (Reynolds, 1988) are widespread in the region, erosion has removed them from the main valleys between Alpine and Nutrioso. As a result, the 1 Alpine-Federal was spudded in sedimentary strata of Oligocene to Eocene age (Reynolds, 1988).
    [Show full text]
  • General Geology of the Franklin Mountains, El Paso County, Texas
    THE GENERAL GEOLOGY OF THE FRANKLIN MOUNTAINS, EL PASO COUNTY, TEXAS EL PASO GEOLOGICAL SOCIETY AND PERMIAN BASIN SOCIETY OF ECONOMIC PALEONTOLOGISTS AND MINERALOGISTS FEBRUARY 24, 1968 Society Members Permian Basin Section El Paso Geological Society Society of Economic Paleontologists and Mineralogists Robert Habbit, President W.F. Anderson, President David V. LeMone, Vice President Richard C. Todd, First Vice President Karl W. Klement, Second Vice President Charles Crowley, Secretary Kenneth O. Sewald, Secretary William S. Strain Gerald L. Scott, Treasurer Editor and Coordinator: David V. LeMone ii TABLE OF CONTENTS Page Introduction ............................................................................. ii Robert Habbit General Geology of the Franklin Mountains: Road Log .......................................... 1 David V. LeMone Precambrian Rocks of the Fusselman Canyon Area ............................................. 12 W.N. McAnulty, Jr. Paleoecology of a Canadian (Lower Ordovician) Algal Complex .................................. 15 David V. LeMone Late Paleozoic in the El Paso Border Region .................................................. 16 Frank E. Kottlowski Late Cenozoic Strata of the El Paso Area ..................................................... 17 William S.Strain A Preliminary Note on the Geology of the Campus “Andesite .................................... 18 Jerry M. Hoffer Conjectural Dating by Means of Gravity Slide Masses of Cenozoic Tectonics of the Southern Franklin Mountains, El Paso County, Texas ..........................................
    [Show full text]
  • NAT ONAL MONUMENT NEW Mexico
    ,1 - /9/93:. 0'7/ -r FECUS NAT ONAL MONUMENT NEW MEXiCO ITS GEOLOGIC SETTING metadc304325 PECOS NATIONAL MONUMENT NEW MEXICO ITS GEOLOGIC SETTING By ROSS B. JOHNSON A description of rocks and landscapes and their effect on man 7 T O CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY BULLETIN 1271-E UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director U.S. GOVERNMENT PRINTING OFFICE, WASHINGTON : 1969 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Introduction_-------------------------------___El Rocks near the monument----------------------2 Geographic extent of the formations of Glorieta Mesa __------------------------------------7 Sources of rock fragments and environments of deposition---------------------------------9 Relation of Glorieta Mesa to the mountains -------- 9 Use of rock products by the Indians and Spanish priests__----------------------------------10 References cited_-----------------------------__11 PLATE 1. Geology and topography of Glorieta Mesa and Pecos National Monument, N. Mex -_ --- In pocket FIGURES Page 1. Map showing location of Glorieta Mesa and Pecos National Monument-----------------E3 2. Photograph showing rock sequence on Glorieta Mesa at Cerro de Escobas------------------4 3. Columnar section of generalized geologic se- quence of rock units on Glorieta Mesa at Cerro de Escobas near Pecos National Monu- ment----------------------------------5 III CONTRIBUTIONS TO GENERAL GEOLOGY
    [Show full text]