From Pilanesberg to Lovozero

**Authors:**Lurie, Jos**Date:**2010-08-05T06:56:40Z**Subjects:**Pilanesberg (South Africa) , Lovozero (Soviet Union) , Geology - Pilanesberg (South Africa) , Mining engineering - South Africa , Alkaline rocks - Pilanesberg (South Africa)**Type:**Inaugural**Identifier:**uj:15076 , http://hdl.handle.net/10210/3374**Description:**Inaugural lecture--Dept. of Engineering, Technikon Witwatersrand, 19 September 2001**Full Text:**

**Authors:**Lurie, Jos**Date:**2010-08-05T06:56:40Z**Subjects:**Pilanesberg (South Africa) , Lovozero (Soviet Union) , Geology - Pilanesberg (South Africa) , Mining engineering - South Africa , Alkaline rocks - Pilanesberg (South Africa)**Type:**Inaugural**Identifier:**uj:15076 , http://hdl.handle.net/10210/3374**Description:**Inaugural lecture--Dept. of Engineering, Technikon Witwatersrand, 19 September 2001**Full Text:**

Lurie and Ponelat's catalogue of symmetrical polyhedra

**Authors:**Lurie, Jos**Date:**2008-09-23T09:53:05Z**Subjects:**symmetrical polyhedra , platonic solids , archimedean polyhedra , crystallography**Type:**Book**Identifier:**uj:1683 , http://hdl.handle.net/10210/1035**Description:**The scope of this catalogue is more-or-less confined to the most symmetrical polyhedra exemplified by the socalled Platonic solids (the five convex forms each of which consists ofaset of identical regular polygon faces) and their symmetry associates including the Archimedean polyhedra. The five solids are the tetrahedron, the hexahedron (cube), the octahedron, the dodecahedron and the icosahedron. These fall into three symmetry groups: tetrahedral, octahedral and icosahedral. The seven members of the last two groups, together with a combination of all, are given on page iv. Because of its relatively low symmetry the tetrahedral group receives somewhat cursory attention. The symmetrical polyhedra described are by no means exhaustive - even with the constraint of considering only the most symmetrical ones there are, in fact infinite possibilities. However, examples produced using several techniques are presented here and these processes (especially producing successive generations) can be employed to produce ever more obscure but highly symmetrical polyhedra. The first contributor to this catalogue had been trained as a draughtsman and had studied crystallography and, having encountered a regular pentagonal dodecahedron for the first time managed, without prior knowledge of them, to produce drawings, applying basic crystallographic principles, of all the Archimedean solids (except the two "snub" forms). The seven forms ofthe icosahedral symmetry group were also produced. Many other symmetrical polyhedra were also "discovered" before being introduced to the Cundy and Rollett classic "Mathematical Models". The logo on the cover of this catalogue was produced by using a stereogram and following Penfield's description but manual draughting of the more complex forms is hugely problematic and the second contributor's role in producing these by computer became indispensable. The computerised portion of the material ofthis catalogue was implemented by Sven Ponelat between October 1993 and April 1997 with the use of an Autocad programme. It largely involved techniques that at the time, had not been used before and, as far as can be established, are little known at present. Fundamentally, it involved utilising the symmetry of a given polyhedron to generate further positions of the polyhedron which can be unioned together. Provided all the components of a given symmetry element are utilised, the resulting compound retains the full symmetry of the starting polyhedron. Thus, partial utilisation of a symmetry element which produces lower symmetry forms is largely omitted. The analysis of the intersections of the compounds generated in terms of their combined convex forms is a new technique apparently. The first author has continued to produce forms up to the present (2007) such as the duals of some forms which have been executed, largely manually, and to systematise the study. Besides utilising a fixed orientation, all combinations and compounds have been rendered in colour to simplify interpretation and comparisons. The analysing of intersections in terms of the components of the combinations so produced apparently has notbeen attempted before.**Full Text:**false

**Authors:**Lurie, Jos**Date:**2008-09-23T09:53:05Z**Subjects:**symmetrical polyhedra , platonic solids , archimedean polyhedra , crystallography**Type:**Book**Identifier:**uj:1683 , http://hdl.handle.net/10210/1035**Description:**The scope of this catalogue is more-or-less confined to the most symmetrical polyhedra exemplified by the socalled Platonic solids (the five convex forms each of which consists ofaset of identical regular polygon faces) and their symmetry associates including the Archimedean polyhedra. The five solids are the tetrahedron, the hexahedron (cube), the octahedron, the dodecahedron and the icosahedron. These fall into three symmetry groups: tetrahedral, octahedral and icosahedral. The seven members of the last two groups, together with a combination of all, are given on page iv. Because of its relatively low symmetry the tetrahedral group receives somewhat cursory attention. The symmetrical polyhedra described are by no means exhaustive - even with the constraint of considering only the most symmetrical ones there are, in fact infinite possibilities. However, examples produced using several techniques are presented here and these processes (especially producing successive generations) can be employed to produce ever more obscure but highly symmetrical polyhedra. The first contributor to this catalogue had been trained as a draughtsman and had studied crystallography and, having encountered a regular pentagonal dodecahedron for the first time managed, without prior knowledge of them, to produce drawings, applying basic crystallographic principles, of all the Archimedean solids (except the two "snub" forms). The seven forms ofthe icosahedral symmetry group were also produced. Many other symmetrical polyhedra were also "discovered" before being introduced to the Cundy and Rollett classic "Mathematical Models". The logo on the cover of this catalogue was produced by using a stereogram and following Penfield's description but manual draughting of the more complex forms is hugely problematic and the second contributor's role in producing these by computer became indispensable. The computerised portion of the material ofthis catalogue was implemented by Sven Ponelat between October 1993 and April 1997 with the use of an Autocad programme. It largely involved techniques that at the time, had not been used before and, as far as can be established, are little known at present. Fundamentally, it involved utilising the symmetry of a given polyhedron to generate further positions of the polyhedron which can be unioned together. Provided all the components of a given symmetry element are utilised, the resulting compound retains the full symmetry of the starting polyhedron. Thus, partial utilisation of a symmetry element which produces lower symmetry forms is largely omitted. The analysis of the intersections of the compounds generated in terms of their combined convex forms is a new technique apparently. The first author has continued to produce forms up to the present (2007) such as the duals of some forms which have been executed, largely manually, and to systematise the study. Besides utilising a fixed orientation, all combinations and compounds have been rendered in colour to simplify interpretation and comparisons. The analysing of intersections in terms of the components of the combinations so produced apparently has notbeen attempted before.**Full Text:**false

Symmetrical polyhedra

**Authors:**Lurie, Jos**Date:**2008-09-23T09:53:32Z**Subjects:**symmetrical polyhedra , crystallography , platonic solids , archimedean polyhedra**Type:**Book**Identifier:**uj:1684 , http://hdl.handle.net/10210/1036**Description:**Much of the material of this book was prepared over a period commencing more than a decade ago and, while a few instances have considered publishing it commercially, the cost in relation to the potential market have been the reason for not implementing this. Over the centuries philosophers and mathematicians have been fascinated by regular polyhedra. Those that have attracted particular attention are essentially isometric1 with high symmetry. It is these and related forms that are largely dealt with in this book. Mathematics necessarily demands a rigid proof of a proposition and a clear distinction between observational evidence and watertight verification. Typical was the proposed solution following three centuries of mathematical endeavour of the close packed spheres problem. Stated simply: what volume is occupied by space in the closest packing of identical solid spheres? Professor Hsiang required one hundred pages of tricky geometry to produce a mathematical solution (apparently not universally accepted) to a problem which the author faced in calculating the theoretical maximum porosity of close-packed equal-sized spheres for an engineering geology text. Doubtless the problem, from different viewpoints, has been faced by others. A practical solution (without mathematical proof was obtained in two hours and using a few lines of simple calculations by converting it into a polyhedral problem! The author was unaware that Kepler had approached the problem originally in this way. Crystallographers are concerned only with those polyhedra whose external form is prescribed by a three dimensional repeating pattern of molecular groups. Excluded is five-fold symmetry and thus consideration of a host of most beautiful polyhedra. Furthermore, only three true stellations are encountered among the crystallographically possible polyhedra. Also, since the development of Xray diffraction, crystallographers have focussed mainly on the internal arrangement patterns of atomic components and interest in external crystal morphology has declined considerably. Through career involvement in mineralogy, chemistry, geology, gemmology and engineering the author was struck by the recurrence in these disciplines of polyhedral phenomena. Perspectives are different but inevitably there is a remarkable convergence when following a particular aspect.**Full Text:**false

**Authors:**Lurie, Jos**Date:**2008-09-23T09:53:32Z**Subjects:**symmetrical polyhedra , crystallography , platonic solids , archimedean polyhedra**Type:**Book**Identifier:**uj:1684 , http://hdl.handle.net/10210/1036**Description:**Much of the material of this book was prepared over a period commencing more than a decade ago and, while a few instances have considered publishing it commercially, the cost in relation to the potential market have been the reason for not implementing this. Over the centuries philosophers and mathematicians have been fascinated by regular polyhedra. Those that have attracted particular attention are essentially isometric1 with high symmetry. It is these and related forms that are largely dealt with in this book. Mathematics necessarily demands a rigid proof of a proposition and a clear distinction between observational evidence and watertight verification. Typical was the proposed solution following three centuries of mathematical endeavour of the close packed spheres problem. Stated simply: what volume is occupied by space in the closest packing of identical solid spheres? Professor Hsiang required one hundred pages of tricky geometry to produce a mathematical solution (apparently not universally accepted) to a problem which the author faced in calculating the theoretical maximum porosity of close-packed equal-sized spheres for an engineering geology text. Doubtless the problem, from different viewpoints, has been faced by others. A practical solution (without mathematical proof was obtained in two hours and using a few lines of simple calculations by converting it into a polyhedral problem! The author was unaware that Kepler had approached the problem originally in this way. Crystallographers are concerned only with those polyhedra whose external form is prescribed by a three dimensional repeating pattern of molecular groups. Excluded is five-fold symmetry and thus consideration of a host of most beautiful polyhedra. Furthermore, only three true stellations are encountered among the crystallographically possible polyhedra. Also, since the development of Xray diffraction, crystallographers have focussed mainly on the internal arrangement patterns of atomic components and interest in external crystal morphology has declined considerably. Through career involvement in mineralogy, chemistry, geology, gemmology and engineering the author was struck by the recurrence in these disciplines of polyhedral phenomena. Perspectives are different but inevitably there is a remarkable convergence when following a particular aspect.**Full Text:**false

The Pilanesberg: geology, rare element geochemistry and economic potential

**Authors:**Lurie, Jos**Date:**2009-02-27T06:00:32Z**Subjects:**actinides , airborne radiometric surveys , alkaline complexes , geochemistry , Ilimaussaq , Khibini , Kola peninsula , lanthanides , Lovozero , lujaurite , nepheline syenites , niobium , Pilanesberg , Prospecting techniques , rare earths , rare elements , ring complexes , rock genetics , rock suite genetics , trace elements**Type:**Book**Identifier:**uj:1689 , http://hdl.handle.net/10210/2188**Description:**The thesis for which a doctorate was awarded by Rhodes University at the beginning of 1974 was: "The Pilanesberg:Geology, Geochemistry and Economic Potential" and it forms a substantial part (65%) of this account. Some of the concepts are possibly somewhat outdated but it is felt that the validity of aspects such as the value of rare element studies for the elucidation of genetic relations between suites of igneous rocks remains. There are several reasons why this expanded version of the thesis has been prepared. Firstly, as one of the classic alkali ring-complexes, there has been a demand for information regarding the Pilanesberg and its geology and over the years the author who holds the copyright has been requested from researchers abroad for permission to obtain copies of the thesis -the most recent in the current year (2004). The majority of these are persons with a particular interest in alkaline rocks. Secondly, the author did considerable additional work on the Complex some of which has appeared in a number of publications all of which are not easily come by at this stage. Included also are some results from a study visit to the alkali massifs of Lovozero and Khibini located on the Kola Peninsula, Russia in 1992. Thirdly, a classification presented was based on all the whole rock analyses presented by previous workers. These analyses are presumably of 27 single samples (nothing in their reports suggest otherwise). Subsequent post-thesis results based on 50 composite serial samples (major units were represented by an average of 30 samples each) were in some respects, in gross contradiction to classification details and other aspects and updating is called for. Fourthly, the account in the thesis ofthe economic potential ofthe Pilanesberg aroused the interest of several mining companies some of whom did considerable additional exploration work. The most important of these in terms of their detailed programmes was, without question, Johanneburg Consolidated Investment. Others were: Newmont Mining and Rio Tinto. Several other companies took an interest but made no contribution in respect of new knowledge. A colleague involved the author in Rare Earths Investment which obtained mineral rights over the more economically interesting areas and which awarded options to companies to do further exploration. Finally, as virtually the whole of the area of the complex has been developed into a game reserve which has developed to the stage of including the "big five" in its game check list, the area is no longer easily accessible for detailed geological work. It seemed a great pity that all the additional information will not be available to researches and others who have interest in this, one of the geological wonders of the world.Some of the previous mapping was again revised,partly by senior students of the Technikon Witwatersrand under the author's supervision just prior to the introduction of lions into the reserve. Localities are still referred to original farm boundaries which no longer exist but for ease of reference are overprinted on the new map and, in addition, to ease the location of points of interest the game tracks established are included as are the positions of geo-sites unfortunately one or two of the descriptions at the sites are incorrect (eg., site 3 is actually located on the Green Foyaite ring and not on a "porphyritic dyke").**Full Text:**

**Authors:**Lurie, Jos**Date:**2009-02-27T06:00:32Z**Subjects:**actinides , airborne radiometric surveys , alkaline complexes , geochemistry , Ilimaussaq , Khibini , Kola peninsula , lanthanides , Lovozero , lujaurite , nepheline syenites , niobium , Pilanesberg , Prospecting techniques , rare earths , rare elements , ring complexes , rock genetics , rock suite genetics , trace elements**Type:**Book**Identifier:**uj:1689 , http://hdl.handle.net/10210/2188**Description:**The thesis for which a doctorate was awarded by Rhodes University at the beginning of 1974 was: "The Pilanesberg:Geology, Geochemistry and Economic Potential" and it forms a substantial part (65%) of this account. Some of the concepts are possibly somewhat outdated but it is felt that the validity of aspects such as the value of rare element studies for the elucidation of genetic relations between suites of igneous rocks remains. There are several reasons why this expanded version of the thesis has been prepared. Firstly, as one of the classic alkali ring-complexes, there has been a demand for information regarding the Pilanesberg and its geology and over the years the author who holds the copyright has been requested from researchers abroad for permission to obtain copies of the thesis -the most recent in the current year (2004). The majority of these are persons with a particular interest in alkaline rocks. Secondly, the author did considerable additional work on the Complex some of which has appeared in a number of publications all of which are not easily come by at this stage. Included also are some results from a study visit to the alkali massifs of Lovozero and Khibini located on the Kola Peninsula, Russia in 1992. Thirdly, a classification presented was based on all the whole rock analyses presented by previous workers. These analyses are presumably of 27 single samples (nothing in their reports suggest otherwise). Subsequent post-thesis results based on 50 composite serial samples (major units were represented by an average of 30 samples each) were in some respects, in gross contradiction to classification details and other aspects and updating is called for. Fourthly, the account in the thesis ofthe economic potential ofthe Pilanesberg aroused the interest of several mining companies some of whom did considerable additional exploration work. The most important of these in terms of their detailed programmes was, without question, Johanneburg Consolidated Investment. Others were: Newmont Mining and Rio Tinto. Several other companies took an interest but made no contribution in respect of new knowledge. A colleague involved the author in Rare Earths Investment which obtained mineral rights over the more economically interesting areas and which awarded options to companies to do further exploration. Finally, as virtually the whole of the area of the complex has been developed into a game reserve which has developed to the stage of including the "big five" in its game check list, the area is no longer easily accessible for detailed geological work. It seemed a great pity that all the additional information will not be available to researches and others who have interest in this, one of the geological wonders of the world.Some of the previous mapping was again revised,partly by senior students of the Technikon Witwatersrand under the author's supervision just prior to the introduction of lions into the reserve. Localities are still referred to original farm boundaries which no longer exist but for ease of reference are overprinted on the new map and, in addition, to ease the location of points of interest the game tracks established are included as are the positions of geo-sites unfortunately one or two of the descriptions at the sites are incorrect (eg., site 3 is actually located on the Green Foyaite ring and not on a "porphyritic dyke").**Full Text:**

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