By Victor Vianu (auth.), Jörg Flum, Mario Rodriguez-Artalejo (eds.)
The 1999 Annual convention of the eu organization for desktop technological know-how good judgment, CSL’99, was once held in Madrid, Spain, on September 20-25, 1999. CSL’99 used to be the thirteenth in a sequence of annual conferences, initially meant as Internat- nal Workshops on laptop technological know-how good judgment, and the eighth to be held because the - nual convention of the EACSL. The convention was once geared up by way of the pc technological know-how Departments (DSIP and DACYA) at Universidad Complutense in M- rid (UCM). The CSL’99 software committee chosen 34 of ninety one submitted papers for p- sentation on the convention and e-book during this court cases quantity. each one submitted paper was once refereed by means of no less than , and in just about all circumstances, 3 di erent referees. the second one refereeing around, formerly required prior to a - according to was once permitted for ebook within the complaints, was once dropped following a choice taken through the EACSL club assembly held in the course of CSL’98 (Brno, Czech Republic, August 25, 1998).
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Additional resources for Computer Science Logic: 13th International Workshop, CSL’99 8th Annual Conference of the EACSL Madrid, Spain, September 20–25, 1999 Proceedings
Weathering, of course, will affect the engineering properties of a rock, and this is dealt with in detail in Chapter 3. An individual rock type or specimen is always described in terms of its mineral composition and its texture, and both are used in the classification of rocks. According to their manner of f formation, rocks are of three main types: Geology for civil engineers 30 Igneous rocks are formed from magma, which has originated well below the surface, has ascended towards the surface, and has crystallised as solid rock either on the surface or deep within the Earth’s crust as its temperature fell.
The dykes of a swarm are parallel or subparallel, except where they are deflected locally by secondary stresses at geological boundaries, such as a major fault. A dyke swarm is sometimes related to a major centre of igneous activity, either by intersecting it, or by spreading out from it. The centre may be the site of one or more major granite plutons. Dykes ‘key in’ to the centre by swinging into trends which are radial from it. The frequency of dykes and the total amount of tensional stretching are greater near the centre.
Amygdales can be distinguished from phenocrysts because of their rounded shape and variation in amount within the rock. 21 Vesicular and amygdaloidal texture in basalt. 22 Ophitic texture. Geology for civil engineers 36 Ophitic texture (Fig. 22) is produced when plagioclase feldspar and augite crystallise at the same time to produce a felted arrangement of interlocking crystals (see Fig. 23). It is normally present in the basic hypabyssal rock dolerite, and is the reason for its high crushing strength, and hence for its suitability as roadstone.
Computer Science Logic: 13th International Workshop, CSL’99 8th Annual Conference of the EACSL Madrid, Spain, September 20–25, 1999 Proceedings by Victor Vianu (auth.), Jörg Flum, Mario Rodriguez-Artalejo (eds.)