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Lamprophyre

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The document discusses lamprophyres, which are ultramafic, mafic, or intermediate intrusive rocks that form dikes or sills at shallow crustal levels. It covers the mineralogy, petrology, classification, occurrence in India, and economic importance of lamprophyres. Lamprophyres are classified into three main types - calc-alkaline, alkaline, and melilitic. Common lamprophyre types discussed include vogesites, minettes, spessartites, and kersantites. Lamprophyres in India are mostly found in Gondwana basins and some alkaline complexes. They can potentially contain diamonds or host gold mineralization.

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SEMINAR ON
1. Introduction 2. Mineralogy 3. Petrology 4. Classification 5. Origin 6. Indian occurrence 7. Economic importance 8. Conclusion 9. Reference
INTRODUCTION  Lamprophyres are generically referred to ultramafic, mafic,(or)intermediate rocks.  That intrude the basement at shallow-crustal levels and form dikes(or)sills.  It has a panidiomorphic granular texture.  Lamprophyres are melanocratic ,porphyritic ,hypabyssal rocks.  Lamprophyres derived from Greek word lampros meaning ‘bright’ and phyro meaning ‘to mix’.
MINERALOGY  The lamprophyres commonly consists of alkali rich calc-alkali to ultramafic minerals.  The essential mineral composition of lamprophyre are Biotite, Amphibole,Pyroxene, plus feldspar and feldspathoids.  The accessory minerals compositions of lamprophyre are Sulphides, zeolites, flourite, iron, titanium, oxides and apatite to quartz(or)olivine.
Petrology Mitchell has suggested that rocks belonging to the lamprophyre facies are characterized by the presence of phenocrysts of mica (or)amphibole together with lesser clinopyroxene melitlite set in a groundmass which may consist of plagioclase, alkali feldspar feldspathoids carbonate monticellite. Any dark intrusive rock in which dark minerals occur both as phenocrysts and as groundmass.
Lamprophyre
CLASSIFICATION Lamprophyre are classified into three types; 1.Calc-alkaline lamprophyres 2. Alkaline lamprophyres 3. Melilitic lamprophyres
Light colored constituents Predominant mafic minerals feldspar foid Biotite, diopsidic augite,(± olivine) Hornblende, diopsidic augite, (± olivine) Na-Ti- amphiboles, Ti-augite, olivine, biotite Melilite, biotite ±Ti- augite ± olivine ± calcite or > pl pl > or or > pl pl > or - - - - feld > foid feld > foid glass or foid - Minette kersantite Vogesite spessartite Sannaite Camptonite Monchiquit e Polzenite alnoite Lamprophyre branch: Calc-alkaline Alkaline Melilitic The lamprophyres that belong to these groups, and the mineral characteristics of each, as recommended by the IUGS, are given in the following table.
CALC-ALKALINE LAMPROPHYRES  The calc-alkaline lamprophyres are the common lamprophyres and often described as ordinary lamprophyres. This four lamprophyres are most readily classified using modal data: Vogesites: From Vosges in Northern France. A vogesite is a porphyritic alkaline igneous rock dominated by essential amphibole, usually hornblende, and potassic feldspar, often with augite and plagioclase present as accessories within the groundmass.
Minettes: From an old term used by miners in the Vosges, are alkali-feldspar. A minette is a porphyritic alkaline igneous rock dominated by essential biotite and potassic feldspar, often with augite and plagioclase present as accessories within the groundmass. Spessartites: From Spessart mountains in Germany. A spessartite is a porphyritic alkaline igneous rock dominated by essential amphibole, usually hornblende, and plagioclase feldspar, often with augite present as an accessory. Plagioclase occurs in the groundmass and potassic feldspar is absent or present in low abundance. Kersantites: From Kersanton, a village in France, are Plagioclase, Honrblende, Augite lamprophyres.
ALKALINE &MELILITIC LAMPROPHYRES  The alkaline and melilitic lamprophyres will be considered together.  Because both groups contain alkaline rocks and are usually associated with alkaline complexes and the rocks of the carbonatite-nepheline- ijolite association.  The common alkaline lamprophyres are comptonites, sannaites, and monchiquites and they are chemically akin to alkaline Basalt, Basanites and Nephelinites.
Monchiquites: From Sierra de Monchique in Southern Portugal. A monchiquite is a porphyritic alkaline igneous rock dominated by essential olivine, titanaugite and brown hornblende. From Campton in the New Hampshire (USA). A camptonite is a porphyritic alkaline igneous rock dominated by essential plagioclase and brown amphibole, usually hornblende, often with titanaugite. Plagioclase occurs in the groundmass. Comptonite: Sannaites: From Sannavand, Fen complex, Sweden. Sannaites are broadly to Comptonites, except that they contain alkali feldspar in place of plagioclase.
Polenzite: From Polzen area of the Bohemian massif, Czechoslovakia. Is a melilitic lamprophyre that usually contain between 10-30% of feldspathoids (Nepheline and Hauyne) and it normally contains the same minerals as occur in alnöite. Alnoite; From Alno island, Sweden. A alnoite is a porphyritic alkaline igneous rock dominated by essential olivine, biotite and pyroxene, in a groundmass containing melilite. It can contain monticellite.
The essential components in lamprophyre genesis are;  High depth of melting  Which yields more mafic magmas  Low degrees of partial melting  which yields magmas rich in the alkalis (particularly potassium)
 To provide the biotite (phlogopite) and amphibole (pargasite) mineralogy lack of fractional crystallisation  High potassium and sodium concentrations (silica undersaturation is common) some form of volatile enrichment  Lithophile element (K, Ba, Cs, Rb) enrichment, high Ni and Cr, Cont. d
DISTRIBUTION  Lamprophyres are usually associated with voluminous granodiorite intrusive episodes. They occur as marginal facies to some granites, though usually as dikes and sills marginal to and crosscutting the granites and diorites. In other districts where granites are abundant no rocks of this class are known. It is rare to find only one member of the group present, but minettes, vogesites, kersantites, etc., all appear and there are usually transitional forms.  Lamprophyres are also known to be spatially and temporally associated with gold mineralisation. The more reasonable explanation for the correlation is that lamprophyres, representing "wet" melts of the asthenosphere and mantle, correlate with a period of high fluid flow from the mantle through the crust, during subduction-related metamorphism, which drives gold mineralisation.
INDIAN OCCURRENCE  In INDIA lamprophyres are mostly from the gondwana basins. Although they have been reported from some younger alkaline complexes also.  From raniganj coal field minette and kersantite are the most frequently reported types  Calc-alkali lamprophyres are reported from mundwana complex of RAJASTHAN  Amba-dongar carbonatite complex of GUJARAT is intruded by camptonite and kersantite
Lamprophyre
ECONOMIC IMPORTANCE The economic importance of ultrapotassic rocks is wide and varied. Kimberlites, lamproites and perhaps even lamprophyres are known to contain diamond. These rocks are all produced at depths in excess of 120 km and thus can bring diamond to the surface as xenocrysts Ultrapotassic granites are a known host for much granite-hosted gold mineralisation. Significant porphyry-style mineralisation is won from highly potassic to ultrapotassic granites. Ultrapotassic A-type intracontinental granites may be associated with fluorite and columbite – tantalite mineralization.
CONCLUSION  Lamprophyres are melanocratic ,porphyritic, hypabyssal rocks.  The lamprophyres commonly consists of alkali rich calc-alkali to ultramafic minerals.  In INDIA lamprophyres are mostly from the gondwana basins. Although they have been reported from some younger alkaline complexes also. The economic importance of ultrapotassic rocks is wide and varied.
Reference BOOKS ;  Donald W. Hyndman ,(1976),petrology of igneous and metamorphic rocks, Mcgraw-Hill books, p;366-369  Mihir k. Bose, (1997) igneous petrology, the world press private limited calcutta, p;187-190  www.geology.com  www.wikipediia.com WEBSITES ;
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Lamprophyre

  • 2. 1. Introduction 2. Mineralogy 3. Petrology 4. Classification 5. Origin 6. Indian occurrence 7. Economic importance 8. Conclusion 9. Reference
  • 3. INTRODUCTION  Lamprophyres are generically referred to ultramafic, mafic,(or)intermediate rocks.  That intrude the basement at shallow-crustal levels and form dikes(or)sills.  It has a panidiomorphic granular texture.  Lamprophyres are melanocratic ,porphyritic ,hypabyssal rocks.  Lamprophyres derived from Greek word lampros meaning ‘bright’ and phyro meaning ‘to mix’.
  • 4. MINERALOGY  The lamprophyres commonly consists of alkali rich calc-alkali to ultramafic minerals.  The essential mineral composition of lamprophyre are Biotite, Amphibole,Pyroxene, plus feldspar and feldspathoids.  The accessory minerals compositions of lamprophyre are Sulphides, zeolites, flourite, iron, titanium, oxides and apatite to quartz(or)olivine.
  • 5. Petrology Mitchell has suggested that rocks belonging to the lamprophyre facies are characterized by the presence of phenocrysts of mica (or)amphibole together with lesser clinopyroxene melitlite set in a groundmass which may consist of plagioclase, alkali feldspar feldspathoids carbonate monticellite. Any dark intrusive rock in which dark minerals occur both as phenocrysts and as groundmass.
  • 7. CLASSIFICATION Lamprophyre are classified into three types; 1.Calc-alkaline lamprophyres 2. Alkaline lamprophyres 3. Melilitic lamprophyres
  • 8. Light colored constituents Predominant mafic minerals feldspar foid Biotite, diopsidic augite,(± olivine) Hornblende, diopsidic augite, (± olivine) Na-Ti- amphiboles, Ti-augite, olivine, biotite Melilite, biotite ±Ti- augite ± olivine ± calcite or > pl pl > or or > pl pl > or - - - - feld > foid feld > foid glass or foid - Minette kersantite Vogesite spessartite Sannaite Camptonite Monchiquit e Polzenite alnoite Lamprophyre branch: Calc-alkaline Alkaline Melilitic The lamprophyres that belong to these groups, and the mineral characteristics of each, as recommended by the IUGS, are given in the following table.
  • 9. CALC-ALKALINE LAMPROPHYRES  The calc-alkaline lamprophyres are the common lamprophyres and often described as ordinary lamprophyres. This four lamprophyres are most readily classified using modal data: Vogesites: From Vosges in Northern France. A vogesite is a porphyritic alkaline igneous rock dominated by essential amphibole, usually hornblende, and potassic feldspar, often with augite and plagioclase present as accessories within the groundmass.
  • 10. Minettes: From an old term used by miners in the Vosges, are alkali-feldspar. A minette is a porphyritic alkaline igneous rock dominated by essential biotite and potassic feldspar, often with augite and plagioclase present as accessories within the groundmass. Spessartites: From Spessart mountains in Germany. A spessartite is a porphyritic alkaline igneous rock dominated by essential amphibole, usually hornblende, and plagioclase feldspar, often with augite present as an accessory. Plagioclase occurs in the groundmass and potassic feldspar is absent or present in low abundance. Kersantites: From Kersanton, a village in France, are Plagioclase, Honrblende, Augite lamprophyres.
  • 11. ALKALINE &MELILITIC LAMPROPHYRES  The alkaline and melilitic lamprophyres will be considered together.  Because both groups contain alkaline rocks and are usually associated with alkaline complexes and the rocks of the carbonatite-nepheline- ijolite association.  The common alkaline lamprophyres are comptonites, sannaites, and monchiquites and they are chemically akin to alkaline Basalt, Basanites and Nephelinites.
  • 12. Monchiquites: From Sierra de Monchique in Southern Portugal. A monchiquite is a porphyritic alkaline igneous rock dominated by essential olivine, titanaugite and brown hornblende. From Campton in the New Hampshire (USA). A camptonite is a porphyritic alkaline igneous rock dominated by essential plagioclase and brown amphibole, usually hornblende, often with titanaugite. Plagioclase occurs in the groundmass. Comptonite: Sannaites: From Sannavand, Fen complex, Sweden. Sannaites are broadly to Comptonites, except that they contain alkali feldspar in place of plagioclase.
  • 13. Polenzite: From Polzen area of the Bohemian massif, Czechoslovakia. Is a melilitic lamprophyre that usually contain between 10-30% of feldspathoids (Nepheline and Hauyne) and it normally contains the same minerals as occur in alnöite. Alnoite; From Alno island, Sweden. A alnoite is a porphyritic alkaline igneous rock dominated by essential olivine, biotite and pyroxene, in a groundmass containing melilite. It can contain monticellite.
  • 14. The essential components in lamprophyre genesis are;  High depth of melting  Which yields more mafic magmas  Low degrees of partial melting  which yields magmas rich in the alkalis (particularly potassium)
  • 15.  To provide the biotite (phlogopite) and amphibole (pargasite) mineralogy lack of fractional crystallisation  High potassium and sodium concentrations (silica undersaturation is common) some form of volatile enrichment  Lithophile element (K, Ba, Cs, Rb) enrichment, high Ni and Cr, Cont. d
  • 16. DISTRIBUTION  Lamprophyres are usually associated with voluminous granodiorite intrusive episodes. They occur as marginal facies to some granites, though usually as dikes and sills marginal to and crosscutting the granites and diorites. In other districts where granites are abundant no rocks of this class are known. It is rare to find only one member of the group present, but minettes, vogesites, kersantites, etc., all appear and there are usually transitional forms.  Lamprophyres are also known to be spatially and temporally associated with gold mineralisation. The more reasonable explanation for the correlation is that lamprophyres, representing "wet" melts of the asthenosphere and mantle, correlate with a period of high fluid flow from the mantle through the crust, during subduction-related metamorphism, which drives gold mineralisation.
  • 17. INDIAN OCCURRENCE  In INDIA lamprophyres are mostly from the gondwana basins. Although they have been reported from some younger alkaline complexes also.  From raniganj coal field minette and kersantite are the most frequently reported types  Calc-alkali lamprophyres are reported from mundwana complex of RAJASTHAN  Amba-dongar carbonatite complex of GUJARAT is intruded by camptonite and kersantite
  • 19. ECONOMIC IMPORTANCE The economic importance of ultrapotassic rocks is wide and varied. Kimberlites, lamproites and perhaps even lamprophyres are known to contain diamond. These rocks are all produced at depths in excess of 120 km and thus can bring diamond to the surface as xenocrysts Ultrapotassic granites are a known host for much granite-hosted gold mineralisation. Significant porphyry-style mineralisation is won from highly potassic to ultrapotassic granites. Ultrapotassic A-type intracontinental granites may be associated with fluorite and columbite – tantalite mineralization.
  • 20. CONCLUSION  Lamprophyres are melanocratic ,porphyritic, hypabyssal rocks.  The lamprophyres commonly consists of alkali rich calc-alkali to ultramafic minerals.  In INDIA lamprophyres are mostly from the gondwana basins. Although they have been reported from some younger alkaline complexes also. The economic importance of ultrapotassic rocks is wide and varied.
  • 21. Reference BOOKS ;  Donald W. Hyndman ,(1976),petrology of igneous and metamorphic rocks, Mcgraw-Hill books, p;366-369  Mihir k. Bose, (1997) igneous petrology, the world press private limited calcutta, p;187-190  www.geology.com  www.wikipediia.com WEBSITES ;