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         Faults Geology:     more books (100)
  1. Constraints on the latest movements on the Melones fault zone, Sierra Nevada foothills, California (Shorter contributions to stratigraphy and structural geology) by J. Alan Bartow, 1980
  2. Geology west of the Melones Fault between the feather and Yuba Rivers (Geological Survey professional paper ; 1170-A) by Anna Martha Hietanen, 1980
  3. Geology of faults exposed in trenches in Crater Flat, Nye County, Nevada (Open-file report / United States Department of the Interior, Geological Survey) by W. C Swadley, 1983
  4. NBMG open file report by John W Bell, 1982
  5. Notes on the geology of Ridge Basin and the San Gabirel [i.e. Gabriel] fault zone by John C Crowell, 1952
  6. Quaternary geology and seismic hazard of the Sierra Madre and associated faults: Western San Gabriel Mountains, California by Richard Crook, 1978
  7. Field guide to the geology of the eastern San Gabriel Mountains & San Andreas Fault in the Cajon Pass area, Southern California by Richard Hazlett, 1995
  8. Geology of the White Thorn Fault in northern Christian County, Kentucky;: A paper read before the Geological Society of America at Tuscaloosa, Alabama, May 1, 1958 by Willard Rouse Jillson, 1958
  9. Geology and fault activity of the Lake Hughes segment of the San Andreas Fault zone, Los Angeles County, California: Final technical report (part 2 of ... 1978 to January 26, 1979) (Open file report) by David J Beeby, 1979
  10. Preliminary report on the geology of the Laur-Dingalan fault zone, Luzon, Philippines (Report of investigation - Philippines Bureau of Mines) by R. W. R Rutland, 1967
  11. Subsurface geology of the San Gabriel, Holser, and Simi-Santa Rosa Faults, Transverse Ranges, California: November 1, 1973 to January 31, 1980 : final ... report, contract number 14-08-0001-16747 by Robert S Yeats, 1981
  12. The Wellington Mohaka and Wairarapa faults (Publication of Geology Department, Victoria University of Wellington) by R. H Grapes, 1984
  13. Geology, seismic hazard, and ground-rupture hazard of the San Gabriel and Holser faults, eastern Ventura and western Soledad basins, California: Final technical report by Robert S Yeats, 1983
  14. Fault tectonics: A syllabus for instruction in Department of Geology at the Institut Teknologi, Bandung, Indonesia by Mason L Hill, 1976

101. Engineering Geologic Environment And Sustainable Development
Development I Engineering Geologic Investigation of Active faults Key words engineering geologic environment;engineering seism; active fault;
http://www.pku.edu.cn/academic/xb/96/e96410.html

102. Geology Of Baja California
BAJA CALIFORNIA can be divided into 5 provinces based on geologic landforms. They are. the tilted granitic fault blocks of the main mountain ranges,
http://math.ucr.edu/ftm/bajaPages/Geology.html
Return to Contents Page Printer friendly version >> This page was generously contributed by John Minch, Edwin Minch and Jason Minch in response to a query of mine. They have provided a brief summary of the geology of Baja California.
The three contributors are authors of a recent book "Roadside Geology and Biology of Baja California." (See the Books Page for information on this book).
Fred Metcalf
Page Contents Geologic Provinces Geologic History Baja California Information Pages
Brief Summary of the Geology
of Baja California
by
John Minch, Edwin Minch, and Jason Minch
Geologic Provinces of Baja California
Next
Back to Page Contents
B AJA CALIFORNIA
can be divided into 5 provinces based on geologic landforms. They are:
  • the tilted granitic fault blocks of the main mountain ranges,
  • the broad flat coastal plains,
  • the isolated coastal mountains,
  • the fault block mountains and alluviated valleys of the Basin and Ranges, and
  • the plateaus of the Volcanic Tablelands. The first three provinces are part of the Cretaceous collision of the North American and the Pacific Plate. The last two provinces are directly related to the opening of the Gulf of California.
  • The tilted granitic fault blocks are represented by the Sierra Juarez and the Sierra San Pedro Martir which form the main granitic ranges of the State of Baja California and the Sierra La Laguna of the Cape region mountains. The main rock types in this province are granitic, metamorphic, and metavolcanic.
  • 103. Red River And Associated Faults, Yunnan Province, China: Quaternary Geology, Sli
    The Geological Society of America advancing the geosciences, The 900km-long right-slip Red River fault of southernmost China and northern Vietnam is
    http://www.gsajournals.org/gsaonline/?request=get-abstract&doi=10.1130/0016-7606

    104. SF Bay Images
    Active faults (which slipped during the past 10000 years) are from CW of these images on the web to make geological and seismological information
    http://www.sfbayquakes.org/thumbnails.html
    Thumbnails Map View North View West View East View ... Links These fantastic images are available as a map view or as perspective views looking North, East or West. We also have close ups of different places of interest in the area. Developed by Robert E. Crippen (JPL) and Ross Stein (USGS) these images drape Landsat TM satellite imagery over Digital Elevation Models to show the bay as it has never been seen before. The vertical exaggeration in the oblique views is three times; the view angle is 20 degrees below the horizontal. Active faults (which slipped during the past 10,000 years) are from C.W Jennings, Fault Activity Map of California (1994). The offshore portion of the San Gregorio fault is modified after M.L. Zoback et al (Journal of Geophysical Research v.104, 1999). All the images can be downloaded quickly for printing from your home computer on US Letter paper. Full size 6ft images can be downloaded or ordered from Digital Prism or Kinko's from this site, or you can take a file to any good copy service bureau that offers a poster printing service Click on an image below.

    105. Northernminer.com - The Northern Miner - 9/21/2005
    geology 101 Oil Gas Alternatively, if the fault/fracture cuts a rock at a level close to the earth s surface, then it does not have the same
    http://www.northernminer.com/Tools/Geology101/geo101.asp
    @import url(/common.css); @import url(/Styles/main.css); News Search Advanced Search Page The Northern Miner Home / Daily News Press Release Wires Feature Stories Headlines ... Archives Corporate Data Organization Search Property Search People Search Country Search Investment Metals Commentary Investment Commentary Newsletter Writers Features Katrina: The
    Canadian Impact
    Technology for Business Supplier Information Suppliers Directory Product Specs Product Catalogue Industry Resources Events News and Wire Services Mailing Lists Bullboards Commerce Classifieds Web Services Links Company Links Supplier Links Junior Mining Co. Profiles Industry Related Links Tools Toolbox Mining Dictionary Geology 101 Geology 101 Index
  • Epithermal deposits, Part 1, April 7, 1997 Epithermal deposits, Part 2, April 14, 1997 Quartz-Carbonate vein gold deposits, Part 1, July 28, 1997 Quartz-Carbonate vein gold deposits, Part 2, August 4, 1997 ... Besshi-type VMS deposits (Part II), July 10-16, 2000
  • April 7, 1997
    Epithermal deposits, Part 1

    106. BULLETIN OF THE GEOLOGICAL SURVEY OF JAPAN
    Analyses of active faults in shallow marine and lake areas case studies and of active faults are reviewed regarding the geological setting of shallow
    http://www.aist.go.jp/GSJ/PSV/Pub/gsj_pube/bull/vol51e/vol51_23.htm
    http://www.aist.go.jp/
    webmaster@aist.go.jp ŒÂlî•ñ•ÛŒì index Vol. 51 Japanese Index Special Issue: Evaluation of earthquake potential in offshore areas - reviews of geological approaches - Analyses of active faults in shallow marine and lake areas -case studies and arguments about what to do- Identification of offshore active faults on seismic profiles - application of fault related fold, growth strata and growth triangle - Initiation processes of turbidity currents: implications for assessment of recurrence intervals of offshore earthquakes using turbidites Paleoseismicity analysis using earthquake-induced sediments ... Interaction between subducting seamounts and overriding forearc wedges, and its relation to large earthquakes: a review Analyses of active faults in shallow marine and lake areas -case studies and arguments about what to do- Kohsaku ARAI(Marine Geology Department, GSJ) vol. 51 (2/3) P.49-58 5 figs Keywords: active fault, shallow marine, bay, lake, seismic survey Identification of offshore active faults on seismic profiles - application of fault related fold, growth strata and growth triangle - Yukinobu OKAMURA(Marine Geology Department, GSJ)

    107. Did You Know That Pine Moutain Has Moved?
    Educational page about the geologic history of the Pine Mountain Thrust Fault, in southeastern Kentucky. A thrust fault is a tear in the upper part of the
    http://www.uky.edu/KGS/education/pinemountain.html
    KGS Home Earth Science Education
    Did You Know That Pine Moutain Has Moved?
    Pine Mountain, in the southeastern corner of Kentucky, sits atop the Pine Mountain Thrust Fault. A thrust fault is a tear in the upper part of the Earth's crust along which one block of strata is pushed up and over another block of strata. This is a different kind of movement than the normal faults of the New Madrid Fault Zone (in the Jackson Purchase of western Kentucky), in which movement along the fault is vertical and one block drops down relative to the other, or strike-slip faults like the San Andreas Fault Zone in California, in which movement is in a lateral direction, with one block sliding past the other. Geologists can trace the amount of movement on the fault. The northern portion of Pine Mountain, north of the town of Louellan, has been thrust 4 miles (6.4 km) from its original position. The southern edge in Tennessee has been moved 11 miles (17.6 km)! The area that is now the city of Harlan has been moved 6 to 8 miles from where it started. If you live in Harlan, don't worry, movement along the fault stopped millions of years ago. References that include information about Pine Mountain. If your library does not have these references, they are available from the

    108. Earth Sciences Research
    Principal areas of research the causes and consequences of fault Involved in a collaborative project with the British Geological Survey as part of
    http://www.dur.ac.uk/geolsci.www/research/structural/struct_index.htm
    Home News People Alumni ... Calendar Earth Sciences
    Research Pages Current Research Areas:
    Structural Geology
    Dr R E Holdsworth (Professor)
    Principal areas of research: the causes and consequences of fault reactivation and long-term weakness; the spatial attributes and growth of faults; strain partitioning in regions of oblique convergence/divergence; flow kinematics in crustal and mantle deformation zones. Bob is also the founder of the Reactivation Research Group. more..
    Dr K J W McCaffrey (Senior Lecturer)
    more..
    Dr J Imber (Statoil Lecturer)
    Currently working on a NERC Ocean Margins LINK project that aims to quantify the influence of basement fault reactivation in passive margin settings. This research will compare the growth of fault systems in which there is clear basement involvement with that of ‘thin-skinned’ fault systems using high quality 2D/3D seismic data from various NE Atlantic margin basins. Other research interests include: (1) modelling relay zones on normal faults using 3D distinct element techniques; (2) constraining the thermal and rheological evolution of basement faults using finite difference models; and (3) the interaction between tectonics and sedimentation in growth faulted terranes.

    109. Encyclopedia: Geologic Fault
    Appalachian geologic fault Image copyleft Image taken by me, A transform fault is a geological fault that is a special case of strikeslip faulting
    http://www.nationmaster.com/encyclopedia/Geologic-fault

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    Encyclopedia: Geologic fault
    Updated 87 days 21 hours 41 minutes ago. Other descriptions of Geologic fault Old fault exposed by roadcut near Harrisburg, Pennsylvania . Such faults are common in the folded Appalachians In geology faults are discontinuities (cracks) in the Earth's crust that are the result of differential motion within the crust. Faults are the source of many earthquakes that are caused by slippage vertically or laterally along the fault. The largest examples are at tectonic plate boundaries, but many small faults are known to exist that are far from active plate boundaries. Appalachian geologic fault Image copyleft: Image taken by me, released under GFDL Pollinator 05:52, Sep 19, 2004 (UTC) File history Legend: (cur) = this is the current file, (del) = delete this old version, (rev) = revert to this old version. ... Harrisburg is the capital of Pennsylvania, a state of the United States of America. ...

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