NADM Variant Fact Sheet |
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Variant Name: Cordlink v5.2 | |
Document written by: Eric Boisvert, LCNP, Geological Survey of Canada | |
Eboisver@nrcan.gc.ca | http://www.cgq-qgc.ca/lcnp |
Author: | Brodaric, B., Journeay, M., Talwar, S., and Boisvert, E., |
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Agency: | Geological Survey of Canada |
Date: | 1999 |
URL: | http://132.156.108.208/Cordlink1/ |
In NADM 4.3, SOAs and COAs have their own set of tables that describe them. In CORDLink 5.2, attribute tables for SOAs and COAs are merged into a common pool of shared descriptions..
The way the attributes are now modelled suggests a different cardinality for spatial objects. In 4.3, the implicit cardinality is 1 spatial object = 1 attribute record of a specific type (i.e. 1 polygon in the SHP file is related to a single row of attributes in an SOA table). For example, a single station having more than one structural measurement would require the creation of as many point objects (spatial objects) as there are measurements. In CORDLink 5.2, attribute tables shared between both SOA and COA require special mechanism for the relation. The linkage of attributes with either COAs or SOAs is done through "description" tables, which are essentially relational "bridges" or a "correlation tables". The COA_Description table matches a COA on one side and an attribute in any of the attribute tables on the other side. On the SOA side, the SOA table plays the same role (Appendix 1).See example in Appendix 2 (PDF)
The example is based on a legend description extracted from :Harald Drewes. 1998,. ARIZONA. Geologic map of the Bartlett Mountain Quadrangle, Pima and Santa Cruz counties, Arizona, I-2624. Lat 31 deg 22'30" to 31 deg 30', long 111 deg 15' to 111 deg 22'30". Scale 1:24,000 (1 inch = 2,000 feet). Sheet 43 by 39 1/2 inches.The text of the legend reads as follow :
Dacitic Vent Breccia (Miocene) -Light-medium-gray, finely porphyritic dacitic rock containing inclusions of Jurassic or Proterozoic granite and Jurassic rhyolite (welded tuff?) as much as 20 m in diameter. The subcircular outcrop mass of breccia probably is a volcanic vent or throat. A halo of strongly saussuritized rock 0.3 -0.5 km wide (delineated on map) surrounds this vent. The dacitic matrix consists of phenocrysts (25-35%, as much as 2 mm in length) set in a cryptocrystalline granular groundmass. Phenocrysts included albitized(?) plagioclase (12-18%), chloritized biotite (2-5%), uralized amphibole (2-10%), magnetite (trace to 2%), and apatite (trace). Quartz is present as a secondary mineral, filing vugs.