TSO710/ NTERNATIONAL STANDARD INTERNATIONAL ORGANIZATION FOR STANDARDIZATION MEKJYHAPOJIHA OPTAHW3ALIMA IO CTAHJIAPTVW3ALIMH·ORGANISATION INTERNATIONALE DE NORMALISATION Graphical symbols for use on detailed maps, plans and geological cross-sections -- Part Ill : Representation of magmatic rocks Symboles graphiques a utiliser sur lescartes,les plans etles coupes geologiques detailles Partie Ill:Representationdes rochesmagmatiques First edition-1974-09-15 ANsi Internat Doc Sect SEP 121974 ISO 710/111-1974 (E) UDC526.89:003.62 Ref.No.ISO 710/lll-1974 (E) Descriptors : geology, maps, drawings, transverse sections, igneous rocks, symbols, graphical symbols. Price based on 6 pages Copyright Interm ational Organization for Standardization se from IHS Not for Resale FOREWORD Iso (the International Organization for Standardization) is a worldwide federation of national standards institutes (Iso Member Bodies).The work of developing International Standards is carried out through ISo Technical Committees. Every Member Body interested in a subject for which a Technical Committee has been set up has the right to be represented on that Committee. International organizations, governmental and non-governmentat,in liaison with isO,also takepart inthe work. Draft International Standards adopted by the Technical Committees are circulated to the Member Bodies for approval before their acceptance as International Standards by the ISO Council. Prior to 1972, the results of the work of the Technical Committees were published as Iso Recommendations; these documents are now in the process of being transformed into International Standards.As part of this process, Technical CommitteeISO/TC 82has reviewed ISORecommendation R710/l1l and found it suitable for transformation. International Standard 1so 710/lll therefore replaces ISO Recommendation R710/1l1-1970. ISO Recommendation R710/ll was approved by the Member Bodies of the following countries : Australia Greece Spain Belgium Sweden Czechoslovakia Iran Turkey Egypt, Arab Rep. of Israel United Kingdom France Italy U.S.S.R. Germany Netheriands The Member Bodies of the following countries expressed disapproval of the Recommendation on technical grounds : Chile New Zealand* Hungary South Africa, Rep. of* Ireland* The Member Body of the following country disapproved the transformation of ISO/R710/lll into an International Standard: Poland Other documents in this series on graphical symbols for use on detailed maps, plans and geological cross-sections include : Part I : General rules of representation. Part ll : Representation of sedimentary rocks. Part IV : Representation of metamorphic rocks. (In preparation.) Part V : Representation of minerals. (In preparation.) Subsequently, these Member Bodies approved the Recommendation. ?International OrganizationforStandardization,1974 Copyright International Organization for Standardization ed without license from IHS Not for Resale ISO710/lII-1974(E) INTERNATIONALSTANDARD Graphical symbols for use on detailed maps, plans and geological cross-sections - Part lll : Representation of magmatic rocks 1 SCOPEANDFIELDOFAPPLICATION 2.1.3 Column 3 is reserved for volcanic rocks. The subdivision corresponds to that of the plutonic rocks. This International Standard provides a series of symbols and ornaments for therepresentation of magmatic rocks on 2.2 Individual symbols detailed maps, especially large-scale maps, plans and geological cross-sections. A distinction in the grain size of rocks can be shown by the smaller or greater size of the individual symbols, for The symbols may be divided in two groups : example, the difference between coarse-grained syenite and fine-grained syenite can be indicated by the difference in 1) main types; size of the same symbol (see figures 1 and 2). 2) varia. They are reproduced in two tables which, being derived +++ from a logical system, may be completed easily in case of FIGURE 1 - Coarse-grained 丰丰 need. syenite FIGURE 2 -- Fine-grain
ISO 710-3 1974 Graphical symbols for use on detailed maps plans and geological cross-sections Part 3 Representation of magmatic rocks
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