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| 02289cam 2200433zi 4500 |
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| 001 | 9.873799 |
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| 003 | CaOODSP |
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| 005 | 20221107164022 |
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| 006 | m o d f |
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| 007 | cr ||||||||||| |
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| 008 | 190529e198906##oncabd #ob f000 0 eng d |
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| 040 | |aCaOODSP|beng|erda|cCaOODSP |
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| 041 | |aeng|bfre |
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| 043 | |an-cn---|an-us-ny |
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| 086 | 1 |aEn13-5/89-144E-PDF |
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| 100 | 1 |aLapcevic, P. A., |eauthor. |
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| 245 | 14|aThe use of short packer spacings to characterize hydraulically open fractures in the Lockport formation, Niagara Falls, New York / |cby P.A. Lapcevic and K.S. Novakowski. |
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| 264 | 1|aBurlington, Ontario : |bNational Water Research Institute, Canada Centre for Inland Waters, |cJune 1989. |
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| 300 | |a1 online resource (17 pages, 25 unnumbered pages) : |billustrations, maps, graphs. |
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| 336 | |atext|btxt|2rdacontent |
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| 337 | |acomputer|bc|2rdamedia |
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| 338 | |aonline resource|bcr|2rdacarrier |
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| 490 | 1 |aNWRI contribution ; |v89-144 |
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| 500 | |a"RRB 89-44." |
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| 500 | |aTitle from cover. |
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| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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| 504 | |aIncludes bibliographical references. |
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| 520 | 3 |a"Two boreholes which were drilled in Niagara Falls, New York, were used to examine the nature of fracturing and fracture permeability in flat-lying sedimentary rock. The boreholes were drilled in the vertical orientation, through the entire length of the Lockport formation, a highly permeable Silurian dolostone. The study was conducted in cooperation with the U.S. Geological Survey as part of their ongoing study of the regional groundwater flow system in the Niagara Falls, New York region"--Abstract. |
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| 546 | |aIncludes abstract and management perspective in English and French. |
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| 692 | 07|2gccst|aSedimentary rocks |
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| 693 | 4|aDolomite |
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| 693 | 4|aHydraulic fracturing |
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| 700 | 1 |aNovakowski, Kent S., |eauthor. |
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| 710 | 1 |aCanada. |bEnvironment Canada. |
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| 710 | 2 |aCanada Centre for Inland Waters. |
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| 710 | 2 |aNational Water Research Institute (Canada) |
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| 830 | #0|aNWRI contribution ;|v89-144.|w(CaOODSP)9.844121 |
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| 856 | 40|qPDF|s2.58 MB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en13-5/En13-5-89-144-eng.pdf |
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