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3 edition of Brittle fracture history of the Montague Basin, north-central Massachusetts found in the catalog.

Brittle fracture history of the Montague Basin, north-central Massachusetts

Arthur G. Goldstein

Brittle fracture history of the Montague Basin, north-central Massachusetts

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  • 24 Currently reading

Published by Dept. of Geology and Geography, University of Massachusetts in Amherst .
Written in English

    Places:
  • Massachusetts,
  • Franklin County.
    • Subjects:
    • Faults (Geology) -- Massachusetts -- Franklin County.,
    • Joints (Geology) -- Massachusetts -- Franklin County.

    • Edition Notes

      Statementby Arthur G. Goldstein.
      SeriesContribution - Department of Geology and Geography, University of Massachusetts, Amherst ; no. 25, Contribution (University of Massachusetts at Amherst. Dept. of Geology and Geography) ;, no. 25.
      Classifications
      LC ClassificationsQE606.5.U6 G64 1975
      The Physical Object
      Paginationviii, 108 p. :
      Number of Pages108
      ID Numbers
      Open LibraryOL4377900M
      LC Control Number78621835

      Recommended Citation. Hussey, Arthur M., II and West, David P., Jr, , Bedrock geology of the Brunswick quadrangle, Maine: Maine Geological Survey, Open-File Map Author: Arthur M Hussey Ii, David P West Jr.


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Brittle fracture history of the Montague Basin, north-central Massachusetts by Arthur G. Goldstein Download PDF EPUB FB2

BRITTLE FRACTURE HISTORY OF THE MONTAGUE BASIN, NORTH-CENTRAL MASSACHUSETTS by Arthur G. Goldstein Contribution No. 25 Department of Geology and Geography University of Massachusetts Amherst, Massachusetts July, File Size: 5MB. Eberly, P. O.,Brittle Fracture Petrofabric Along a West-East Traverse From the Connecticut Valley to the Narragansett Basin: MS Thesis, University of Massachusetts, Amherst, Massachusett, USA, p.

Google ScholarCited by: 3. Lithology and fracture characterization from drilling investigations in the Mirror Lake area, Grafton County, New Hampshire (SuDoc I /) [Carole D. Johnson] on *FREE* shipping on qualifying offers.

book. The quadrangle is drained by the east and west branches of the Ware River which join at the Barre Falls Dam to flow southwest out of the area. The Prince, Burnshirt and Canesto Rivers, and Natty Brook, the major tributaries of the Ware River have their headwaters to the north and provide limited exposures of File Size: 9MB.

The Boston basin is one of several late Paleozoic nonmarine sedimentary basins that developed in eastern New England subsequent to the Acadian revolution.

Most of the sedimentary rocks in these basins are known to be Pennsylvanian in age; those in the Boston basin are presumably of this age. A sub–Middle Jurassic unconformity is exhumed at Swift Reservoir, in the Rocky Mountain fold-and-thrust belt of Montana.

The unconformity separates late Mississippian Sun River Dolomite of the Madison Group (ca. Ma) from the transgressive basal sandstone of the Middle Jurassic (Bajocian-Bathonian) Sawtooth Formation (ca. Ma). Late Wisconsinan glacial history of the Connecticut River Valley and a new drainage history of Glacial Lake Hitchcock: varves, landforms, and stratigraphy.

New Englan Intercollegiate Geological Conference Guidebook, 95, B - B Goldstein, A. G., Brittle fracture history of the Montague Basin, north-central Massachusetts. a fracture in which skin is intact at site of fracture is a closed fracture or simple fracture whereas compound fracture or an open fracture is a fracture in which the skin is perforated and there is an open wound down to the site of the fracture.

Chapter 11 Mesozoic tectogenesis: development and deformation of 'Newark' rift zones in the Appalachians (with special emphasis on the Hartford basin, Connecticut) JELLE ZEILINGA DE BOER and AMY E. CLIFFORD ABSTRACT Mesozoic tectogenesis in the Appalachians was dominated by deformation along pre-existing zones of by:   The history of Prescott, Massachusetts; one of four townships in the Swift River Valley which was "born, lived and died" to make way for Metropolitan Water Basin Item Preview remove-circlePages: The NW-trending brittle-ductile shear zones formed at a relatively deep crust level and were subsequently overprinted by the NE-trending brittle fractures and joints at a shallower level (Wang et al., a).

The shear system in the Fengtai district provided the fluid pathway and deposition site for the ore-bearing solutions. The sweet-spot intervals occur mainly at the bottom of the Wufeng-Longmaxi Shale and are 10–40 m in thickness. The sweet-spot interval is characterized by high total organic carbon (TOC) and gas contents, relatively high porosity, high brittle mineral content, and abundant lamination fissures and by: 2.

The MA Geological Survey Department of Geosciences Morrill Science Center University of Massachusetts North Pleasant Street Amherst, MA The Cooper Basin is an intracratonic rift basin of Permian to Triassic age that extends from the north-eastern corner of South Australia into south-western Queensland (McKillop,Gravestock, ) ().The basin covers an area of approximatelykm 2, of which ∼35, km 2 are in NE South Australia.

Three major troughs in the basin, known as the Patchawarra, Nappamerri, and Author: Quaid Khan Jadoon, Eric M. Roberts, Robert A.

Henderson, Thomas G. Blenkinsop, Raphael A.J. Wust. This study is an attempt to unravel the late, brittle deformational history of an area in eastern Connecticut and western Rhode Island.

Brittle petrofabric studies were conducted at outcrops along a 94 kilometer, west-east traverse extending from the Connecticut Valley to the Narragansett Basin (Figures lA and lB). The objective of this study was to investigate the geological controls on stratigraphic and lithologic variability in the Ordovician Utica Shale and related Collingwood Member in the Michigan Basin in order to assess CO 2 sequestration cap rock (seal) potential, including petrophysical properties and mechanical fracture responses.

Twelve conventional cores and hundreds of modern well logs from. For shale of Lower Silurian Longmaxi Formation in Chongqing, southeast Sichuan Basin, characteristics of micro-nano pores in marine shale reservoirs were well studies by means of Field-Emission Scanning Electron Microscope and Low-temperature Low-pressure Adsorption Experiment of CO 2 and N s showed that six types of pore were developed in the shale of Longmaxi Formation, i.e., organic Author: Wenming Ji, Yan Song, Yan Song, Zhenxue Jiang, Mianmo Meng, Qingxin Liu, Fenglin Gao.

[3] As part of this program, a study of predominantly brittle structures (i.e., brittle deformation zones, faults, fractures and associated fault rocks) of the Laxemar‐Simpevarp area was undertaken with the aim to document their character and kinematics, to reconstruct the brittle deformation history of the region and to develop the conceptual model for especially brittle deformation zones Cited by: History of the Town of Hingham, Massachusetts, Volume 2 [Hingham (Mass)., Thomas Tracy Bouv?, Edward Tracy Bouv?] on *FREE* shipping on qualifying offers.

This is a reproduction of a book published before This book may have occasional. Deerfield Basin (Figure 1). A brittle fracture traverse, run in conjunction with this study, is located along the Massachusetts­ Vermont border (Figure 3).

It runs from the Taborton-Grafton area of New York state to the area of Northfield, Massachusetts-Hinsdale, New Size: 4MB. Geologic History of Cape Cod, Massachusetts: USGS General Interest Publication [United U.S. Department of the Interior] on *FREE* shipping on qualifying offers. Cape Cod, a sandy peninsula built mostly during the Ice Age, juts into the Atlantic Ocean like a crooked arm.

Because of its exposed locationFormat: Paperback. T he W itwatersrand has been the main source of world gold throughout the twentieth century, and in many of these years it has accounted for more than half of the world's gold production (Fig.

1).A total of 48, tonnes of gold has been produced since the discovery of these gold fields in Uranium has been a very important byproduct of gold mining since ; the cumulative production of. Geologic History of Cape Cod, Massachusetts Paperback – January 1, by Robert N. Oldale (Author) See all 2 formats and editions Hide other formats and editions.

Price New from Used from Paperback "Please retry" — Author: Robert N. Oldale. Tectonic Breccia of Metamorphosed Intrusive Igneous Rocks in an Acadian Shear Zone, Brooks Village, North-Central Massachusetts. 43 p. Morton, Peter S., Arthur G. Goldstein has written: 'Brittle fracture history of the Montague Basin, north-central Massachusetts' -- subject(s): Faults (Geology), Joints (Geology) Asked in Authors, Poets, and.

The thermal history demonstrates that two phases of heating (– Ma, 83–38 Ma, depositing) happened to the source rocks, separated by two cooling (–83 Ma, 38–23 Ma, uplifting) events.

Fractures of any one set are not always mineralized, and barren joints are found near veins with the same orientation. This phenomenon was also recognized by Engelder et al. () and Evans ().Author: Mark A. Evans. If the history of the Deerfield basin is similar to the Newark basin, most of the tilting of the strata, and hence most deposition, was over by the Middle Jurassic (~ Ma), during which.

Cenozoic post-collisional brittle tectonic history and stress reorientation in the High Zagros Belt (Iran, Fars Province) Article in Tectonophysics (1) March with 55 Reads.

A late Middle Pennsylvanian flora of the Narragansett basin, Massachusetts. that explore geological history and visit four regional geologic provinces—Blue the GSA Northeastern and North.

: Tack Factory Cemetery And the People Buried at the Border of Middleboro and Lakeville, MA Massachusetts (): Jean A. Douillette: Books5/5(1). LOCATION--Lat 42° 34'", long 72° 34'",(revised) Franklin County, Hydrologic Uniton left bank 75 ft downstream from railroad bridge at Montague City, 1, ft downstream from Deerfield River, and at mile DRAINAGE AREA, mi 2.

PERIOD OF RECORD--Discharge: March to current to Octoberpublished as "at Sunderland.". Hidden History of the Human Race Michael Cremo Foreword by Graham Hancock (Author of Fingerprints of the Gods) It is my great pleasure and honor to introduce this abridged edition of Forbidden Archeology.

Let me say at the outset that I believe this book to be one of the landmark intellectual achievements of the late twentieth Size: 1MB. SURFACE-WATER RECORDS LOCATIONLat 41°18'33", long 74°47'43" referenced to North American Datum ofDingman Township, Pike County, PA, Hydrologic Uniton right bank 1, ft upstream from toll bridge (on U.S.

Route ) between Montague, NJ and Milford, PA, mi downstream from Sawkill Creek, and at river mile The brittle failure of Chengkou shale occurs throughout the exploration and development processes of hydrocarbons. To investigate the failure mechanisms of Chengkou shale and analyze the associated mechanical behavior such as crack initiation, propagation, and coalescence at different stress levels, a series of laboratory experiments were conducted on servo-controlled triaxial cells equipped.

The transition from compression to extension is commonly recorded by the development of characteristic extensional structures and metamorphic assemblages that overprint older collisional features (Platt, ; Vanderhaeghe and Teyssier, ).Examples include overprinting of suture zones by low-angle extensional detachments, and the replacement of high-pressure–low-temperature metamorphic Cited by: 1.

Arthur W. Ord-Hume has written: 'Restoring musical boxes & musical clocks' -- subject(s): Conservation and restoration, Musical clock, Music box 'Joseph Haydn and the mechanical organ.

B.S.,Geology, University of Massachusetts at Amherst. Senior Project: Brittle fracture analysis of western New England Advisor: Dr. Donald U. Wise Professional Interests. Field and structural geology ; Geology and hydrogeology of north-central New Mexico ; Earth science education ; Current Projects.

Understanding the distribution and occurrence of hydrocarbon source and reservoir rocks will aid future exploration. (from the Niobrara Playbook).

Fig. Gravitational heat convection in the mantle is the source of forces that move, bend, and break rocks in the Earth's lithosphere.: Fig. Isostasy: floating wooden blocks of different sizes illustrate how oceanic and continental crustal rocks are at relative isostatic equilibrium floating on the mantle.

Fig. Isostatic rebound caused by the melting of continental glaciers. The Deerfield basin is the erosional remnant of one of these rifts, the exposed North American contingent of which are termed the Newark Supergroup (Figure 2).

The Deerfield basin is connected to the Hartford basin of Connecticut and Massachusetts, and constitutes the northernmost exposures of the Newark Supergroup in the United States.Franklin County, Massachusetts Genealogy and History Volunteers Dedicated to Free Genealogy.Start studying Romeo and juliet (Act 2).

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