Kimberlites and lamproites of the East European Platform: Petrology and geochemistry
Several episodes of kimberlite magmatism occurred in the East European Province (EEP) during a long (about 1.5 Gyr) time period, from the Late Paleoproterozoic (ca. 1.8 Ga) in the Archean Ukrainian and Baltic shields to the Middle Paleozoic (ca. 0.36 Ga) mainly in the Arkhangelsk, Timan, and adjacen...
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Published in | Petrology Vol. 15; no. 4; pp. 315 - 334 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
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Dordrecht
Springer Nature B.V
01.07.2007
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Abstract | Several episodes of kimberlite magmatism occurred in the East European Province (EEP) during a long (about 1.5 Gyr) time period, from the Late Paleoproterozoic (ca. 1.8 Ga) in the Archean Ukrainian and Baltic shields to the Middle Paleozoic (ca. 0.36 Ga) mainly in the Arkhangelsk, Timan, and adjacent regions. Based on the analysis of data on 16 kimberlite occurrences and four lamproite occurrences within the EEP, five time stages can be distinguished; one of them, the Middle Paleozoic stage (Middle Ordovician and Devonian), is the most productive epoch for diamond in the northern hemisphere (EEP, Siberian Craton, and part of the China Craton). The analysis of petrological and geochemical characteristics of kimberlites (lamproites were studied less thoroughly) revealed variations in rock composition and their correlation with a number of factors, including the spatial confinement to the northern or southern Archean blocks of the craton, time of formation of the source of kimberlite melts, contents of volatiles and autoliths, etc. Three petrogeochemical types of kimberlites were distinguished: high-, medium-, and low-Ti (TiO2 > 3 wt %, 1–3 wt %, and <1 wt %, respectively). There are two time intervals of the formation of kimberlite and lamproite sources in the EEP, corresponding to TNd(DM) values of about 2 Ga (up to 2.9 Ga in the Por’ya Guba occurrence) and 1 Ga. The latter interval includes two groups of occurrences with model source ages of about 1 Ga (low-and medium-Ti kimberlites of the Zolotitsa and Verkhotina occurrences) and about 0.8 Ga (high-Ti kimberlites of the Kepino and a number of other occurrences); i.e., there seems to be an evolutionary trend in the composition of kimberlites. Concentric zoning patterns were recognized. The role of the crust in kimberlite sources is discussed; it is assumed that buried remnants of the oceanic lithosphere (megaliths) may underlie whole continents. A unique feature of the composition of low-Ti kimberlites, for instance, kimberlites of the Zolotitsa occurrence (to a smaller extent, medium-Ti kimberlites of the V. Grib pipe) is the distinct depletion of highly charged elements and pronounced negative anomalies of Ti, Zr, Th, U, Nb, and Ta in trace-element distribution patterns, which indicates a contribution of crustal material to the source of these kimberlites. It was shown that autoliths exert a significant influence on the differentiation of kimberlite material, resulting in the enrichment of rocks in the whole spectrum of incompatible elements. It was argued that geochemical criteria can be used together with traditional criteria (including those based on indicator minerals) for the assessment of diamond potential in EEP occurrences. We hope that such a combined approach will yield important outcomes in the future. |
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AbstractList | Several episodes of kimberlite magmatism occurred in the East European Province (EEP) during a long (about 1.5 Gyr) time period, from the Late Paleoproterozoic (ca. 1.8 Ga) in the Archean Ukrainian and Baltic shields to the Middle Paleozoic (ca. 0.36 Ga) mainly in the Arkhangelsk, Timan, and adjacent regions. Based on the analysis of data on 16 kimberlite occurrences and four lamproite occurrences within the EEP, five time stages can be distinguished; one of them, the Middle Paleozoic stage (Middle Ordovician and Devonian), is the most productive epoch for diamond in the northern hemisphere (EEP, Siberian Craton, and part of the China Craton). The analysis of petrological and geochemical characteristics of kimberlites (lamproites were studied less thoroughly) revealed variations in rock composition and their correlation with a number of factors, including the spatial confinement to the northern or southern Archean blocks of the craton, time of formation of the source of kimberlite melts, contents of volatiles and autoliths, etc. Three petrogeochemical types of kimberlites were distinguished: high-, medium-, and low-Ti (TiO2 > 3 wt %, 1–3 wt %, and <1 wt %, respectively). There are two time intervals of the formation of kimberlite and lamproite sources in the EEP, corresponding to TNd(DM) values of about 2 Ga (up to 2.9 Ga in the Por’ya Guba occurrence) and 1 Ga. The latter interval includes two groups of occurrences with model source ages of about 1 Ga (low-and medium-Ti kimberlites of the Zolotitsa and Verkhotina occurrences) and about 0.8 Ga (high-Ti kimberlites of the Kepino and a number of other occurrences); i.e., there seems to be an evolutionary trend in the composition of kimberlites. Concentric zoning patterns were recognized. The role of the crust in kimberlite sources is discussed; it is assumed that buried remnants of the oceanic lithosphere (megaliths) may underlie whole continents. A unique feature of the composition of low-Ti kimberlites, for instance, kimberlites of the Zolotitsa occurrence (to a smaller extent, medium-Ti kimberlites of the V. Grib pipe) is the distinct depletion of highly charged elements and pronounced negative anomalies of Ti, Zr, Th, U, Nb, and Ta in trace-element distribution patterns, which indicates a contribution of crustal material to the source of these kimberlites. It was shown that autoliths exert a significant influence on the differentiation of kimberlite material, resulting in the enrichment of rocks in the whole spectrum of incompatible elements. It was argued that geochemical criteria can be used together with traditional criteria (including those based on indicator minerals) for the assessment of diamond potential in EEP occurrences. We hope that such a combined approach will yield important outcomes in the future. Several episodes of kimberlite magmatism occurred in the East European Province (EEP) during a long (about 1.5 Gyr) time period, from the Late Paleoproterozoic (ca. 1.8 Ga) in the Archean Ukrainian and Baltic shields to the Middle Paleozoic (ca. 0.36 Ga) mainly in the Arkhangelsk, Timan, and adjacent regions. Based on the analysis of data on 16 kimberlite occurrences and four lamproite occurrences within the EEP, five time stages can be distinguished; one of them, the Middle Paleozoic stage (Middle Ordovician and Devonian), is the most productive epoch for diamond in the northern hemisphere (EEP, Siberian Craton, and part of the China Craton). The analysis of petrological and geochemical characteristics of kimberlites (lamproites were studied less thoroughly) revealed variations in rock composition and their correlation with a number of factors, including the spatial confinement to the northern or southern Archean blocks of the craton, time of formation of the source of kimberlite melts, contents of volatiles and autoliths, etc. Three petrogeochemical types of kimberlites were distinguished: high-, medium-, and low-Ti (TiO sub(2) > 3 wt %, 1-3 wt %, and <1 wt %, respectively). There are two time intervals of the formation of kimberlite and lamproite sources in the EEP, corresponding to T sub(Nd)(DM) values of about 2 Ga (up to 2.9 Ga in the Por'ya Guba occurrence) and 1 Ga. The latter interval includes two groups of occurrences with model source ages of about 1 Ga (low-and medium-Ti kimberlites of the Zolotitsa and Verkhotina occurrences) and about 0.8 Ga (high-Ti kimberlites of the Kepino and a number of other occurrences); i.e., there seems to be an evolutionary trend in the composition of kimberlites. Concentric zoning patterns were recognized. The role of the crust in kimberlite sources is discussed; it is assumed that buried remnants of the oceanic lithosphere (megaliths) may underlie whole continents. A unique feature of the composition of low-Ti kimberlites, for instance, kimberlites of the Zolotitsa occurrence (to a smaller extent, medium-Ti kimberlites of the V. Grib pipe) is the distinct depletion of highly charged elements and pronounced negative anomalies of Ti, Zr, Th, U, Nb, and Ta in trace-element distribution patterns, which indicates a contribution of crustal material to the source of these kimberlites. It was shown that autoliths exert a significant influence on the differentiation of kimberlite material, resulting in the enrichment of rocks in the whole spectrum of incompatible elements. It was argued that geochemical criteria can be used together with traditional criteria (including those based on indicator minerals) for the assessment of diamond potential in EEP occurrences. We hope that such a combined approach will yield important outcomes in the future. Several episodes of kimberlite magmatism occurred in the East European Province (EEP) during a long (about 1.5 Gyr) time period, from the Late Paleoproterozoic (ca. 1.8 Ga) in the Archean Ukrainian and Baltic shields to the Middle Paleozoic (ca. 0.36 Ga) mainly in the Arkhangelsk, Timan, and adjacent regions. Based on the analysis of data on 16 kimberlite occurrences and four lamproite occurrences within the EEP, five time stages can be distinguished; one of them, the Middle Paleozoic stage (Middle Ordovician and Devonian), is the most productive epoch for diamond in the northern hemisphere (EEP, Siberian Craton, and part of the China Craton). The analysis of petrological and geochemical characteristics of kimberlites (lamproites were studied less thoroughly) revealed variations in rock composition and their correlation with a number of factors, including the spatial confinement to the northern or southern Archean blocks of the craton, time of formation of the source of kimberlite melts, contents of volatiles and autoliths, etc. Three petrogeochemical types of kimberlites were distinguished: high-, medium-, and low-Ti (TiO^sub 2^ > 3 wt %, 1-3 wt %, and <1 wt %, respectively). There are two time intervals of the formation of kimberlite and lamproite sources in the EEP, corresponding to T^sub Nd^(DM) values of about 2 Ga (up to 2.9 Ga in the Por'ya Guba occurrence) and 1 Ga. The latter interval includes two groups of occurrences with model source ages of about 1 Ga (low-and medium-Ti kimberlites of the Zolotitsa and Verkhotina occurrences) and about 0.8 Ga (high-Ti kimberlites of the Kepino and a number of other occurrences); i.e., there seems to be an evolutionary trend in the composition of kimberlites. Concentric zoning patterns were recognized. The role of the crust in kimberlite sources is discussed; it is assumed that buried remnants of the oceanic lithosphere (megaliths) may underlie whole continents. A unique feature of the composition of low-Ti kimberlites, for instance, kimberlites of the Zolotitsa occurrence (to a smaller extent, medium-Ti kimberlites of the V. Grib pipe) is the distinct depletion of highly charged elements and pronounced negative anomalies of Ti, Zr, Th, U, Nb, and Ta in trace-element distribution patterns, which indicates a contribution of crustal material to the source of these kimberlites. It was shown that autoliths exert a significant influence on the differentiation of kimberlite material, resulting in the enrichment of rocks in the whole spectrum of incompatible elements. It was argued that geochemical criteria can be used together with traditional criteria (including those based on indicator minerals) for the assessment of diamond potential in EEP occurrences. We hope that such a combined approach will yield important outcomes in the future.[PUBLICATION ABSTRACT] |
Author | Nosova, A A Kononova, V A Kondrashov, I A Bogatikov, O A |
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Cites_doi | 10.1029/2000JB900439 10.1016/0009-2541(94)00140-4 10.1016/0016-7037(94)90264-X 10.1038/304051a0 10.1016/S0040-1951(96)00230-2 10.34194/ggub.v191.5129 10.1016/0375-6742(94)00018-7 10.1007/s004100050366 10.1007/978-1-4899-0568-0 10.1016/j.lithos.2004.03.047 10.1016/S0040-1951(96)00228-4 10.1007/978-1-4615-1993-5 |
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References | V. A. Kononova (4001_CR23) 2002; 10 R. H. Mitchell (4001_CR32) 1995 M. Heaman (4001_CR15) 2004; 76 S. N. Tsymbal (4001_CR50) 1999; 21 A. V. Samsonov (4001_CR44) 2006 O. A. Bogatikov (4001_CR6) 1991 H. E. O’Brien (4001_CR37) 1999 W. R. Taylor (4001_CR49) 1994; 58 4001_CR52 4001_CR10 4001_CR13 B. A. Mal’kov (4001_CR29) 1995 A.D. Beard (4001_CR4) 1998; 130 4001_CR18 I. M. Artemieva (4001_CR2) 2001; 106 S. M. Jensen (4001_CR19) 2002; 191 V. V. Ushkov (4001_CR53) 2001 R. H. Mitchell (4001_CR33) 1999 A. M. Nikishin (4001_CR34) 1996; 268 J. Ferguson (4001_CR9) 1973 4001_CR21 4001_CR28 V. A. Pervov (4001_CR38) 2002; 386 R. H. Mitchell (4001_CR31) 1986 H. H. Helmstaedt (4001_CR16) 1995; 53 S. N. Tsymbal (4001_CR51) 1999; 21 V. A. Pervov (4001_CR41) 2005 V. A. Pervov (4001_CR39) 2004; 12 Yu. V. Geiko (4001_CR12) 1991; 120 H. H. Helmstaedt (4001_CR17) 1997; 38 V. A. Pervov (4001_CR40) 2005; 400 A. A. Frolov (4001_CR11) 2005 E. V. Yutkina (4001_CR56) 2005; 402 4001_CR5 V. A. Zhuravlev (4001_CR57) 2004 4001_CR3 4001_CR1 O. A. Bogatikov (4001_CR7) 2001; 9 I. P. Pokhilenko (4001_CR42) 2004 E. V. Yutkina (4001_CR55) 2004; 12 N. J. Kusznir (4001_CR25) 1996; 268 4001_CR36 M. M. Kalinkin (4001_CR20) 1993; 1 V. A. Larchenko (4001_CR27) 2005 Yu. Yu. Golubeva (4001_CR14) 2006; 410 N. A. Bozhko (4001_CR8) 2002; 386 L. P. Nikitina (4001_CR35) 1999; 7 V. B. Vasilenko (4001_CR54) 2005 N. V. Sobolev (4001_CR47) 1974 W. F. McDonough (4001_CR30) 1995; 120 C. B. Smith (4001_CR45) 1983; 304 S.-S. Sun (4001_CR48) 1989 4001_CR43 A. V. Lapin (4001_CR26) 2004 V. A. Kononova (4001_CR22) 2000; 372 V. A. Kononova (4001_CR24) 2006; 409 C. B. Smith (4001_CR46) 1985; 88 |
References_xml | – volume: 106 start-page: 16387 year: 2001 ident: 4001_CR2 publication-title: J. Geophys. Res. doi: 10.1029/2000JB900439 contributor: fullname: I. M. Artemieva – start-page: 94 volume-title: Geology and Minerals of Karelia year: 2001 ident: 4001_CR53 contributor: fullname: V. V. Ushkov – volume: 386 start-page: 541 year: 2002 ident: 4001_CR38 publication-title: Dokl. Akad. Nauk contributor: fullname: V. A. Pervov – volume: 120 start-page: 223 year: 1995 ident: 4001_CR30 publication-title: Chem. Geol. doi: 10.1016/0009-2541(94)00140-4 contributor: fullname: W. F. McDonough – volume: 12 start-page: 159 year: 2004 ident: 4001_CR55 publication-title: Petrologiya contributor: fullname: E. V. Yutkina – volume-title: Kimberlites and Related Rocks. Formational Petrogeochemical Criteria year: 2004 ident: 4001_CR26 contributor: fullname: A. V. Lapin – start-page: 222 volume-title: Proceedings of 3th All-Russia Conference on Isotope Geochronology. Isotope Dating of Ore Formation, Magmatism, Sedimentation, and Metamorphism, Moscow, Russia, 2006 year: 2006 ident: 4001_CR44 contributor: fullname: A. V. Samsonov – volume: 372 start-page: 364 year: 2000 ident: 4001_CR22 publication-title: Dokl. Akad. Nauk. contributor: fullname: V. A. Kononova – volume: 58 start-page: 4017 year: 1994 ident: 4001_CR49 publication-title: Geochim. Cosmochim. Acta doi: 10.1016/0016-7037(94)90264-X contributor: fullname: W. R. Taylor – start-page: 135 volume-title: Efficiency of Forecasting and Prospecting of Diamond Deposits: Past, Present, and Future (Diamond 50) year: 2004 ident: 4001_CR57 contributor: fullname: V. A. Zhuravlev – ident: 4001_CR5 – volume: 304 start-page: 51 year: 1983 ident: 4001_CR45 publication-title: Nature doi: 10.1038/304051a0 contributor: fullname: C. B. Smith – ident: 4001_CR1 – ident: 4001_CR13 – volume-title: Deep-Seated Xenoliths in Kimberlites and the Problem of the Composition of the Upper Mantle year: 1974 ident: 4001_CR47 contributor: fullname: N. V. Sobolev – volume: 268 start-page: 237 year: 1996 ident: 4001_CR25 publication-title: Tectonophysics doi: 10.1016/S0040-1951(96)00230-2 contributor: fullname: N. J. Kusznir – volume-title: Volcanic Pipes and Diamond Placers of the Middle Timan year: 1995 ident: 4001_CR29 contributor: fullname: B. A. Mal’kov – volume: 191 start-page: 57 year: 2002 ident: 4001_CR19 publication-title: Geol. Greenland Surv. Bull. doi: 10.34194/ggub.v191.5129 contributor: fullname: S. M. Jensen – start-page: 270 volume-title: Efficiency of Forecasting and Prospecting of Diamond Deposits: Past, Present, and Future (Diamond 50) year: 2004 ident: 4001_CR42 contributor: fullname: I. P. Pokhilenko – volume: 53 start-page: 125 year: 1995 ident: 4001_CR16 publication-title: J. Geochem. Explor. doi: 10.1016/0375-6742(94)00018-7 contributor: fullname: H. H. Helmstaedt – volume: 1 start-page: 205 year: 1993 ident: 4001_CR20 publication-title: Petrologiya contributor: fullname: M. M. Kalinkin – volume: 400 start-page: 88 year: 2005 ident: 4001_CR40 publication-title: Dokl. Akad. Nauk contributor: fullname: V. A. Pervov – start-page: 773 volume-title: Geology of Diamonds: Present and Future year: 2005 ident: 4001_CR54 contributor: fullname: V. B. Vasilenko – start-page: 285 volume-title: Lesotho Kimberlites year: 1973 ident: 4001_CR9 contributor: fullname: J. Ferguson – volume: 130 start-page: 288 year: 1998 ident: 4001_CR4 publication-title: Contrib. Mineral. Petrol. doi: 10.1007/s004100050366 contributor: fullname: A.D. Beard – volume-title: Lamproites year: 1991 ident: 4001_CR6 contributor: fullname: O. A. Bogatikov – volume: 7 start-page: 252 year: 1999 ident: 4001_CR35 publication-title: Petrologiya contributor: fullname: L. P. Nikitina – start-page: 313 volume-title: Magmatism in the Ocean Basins year: 1989 ident: 4001_CR48 contributor: fullname: S.-S. Sun – volume: 9 start-page: 227 year: 2001 ident: 4001_CR7 publication-title: Petrologiya contributor: fullname: O. A. Bogatikov – volume-title: Kimberlites: Mineralogy, Geochemistry and Petrology year: 1986 ident: 4001_CR31 doi: 10.1007/978-1-4899-0568-0 contributor: fullname: R. H. Mitchell – volume: 120 start-page: 52 year: 1991 ident: 4001_CR12 publication-title: Zap. Vses. Mineral. O-va contributor: fullname: Yu. V. Geiko – volume: 410 start-page: 789 year: 2006 ident: 4001_CR14 publication-title: Dokl. Akad. Nauk contributor: fullname: Yu. Yu. Golubeva – ident: 4001_CR10 – start-page: 574 volume-title: Proceedings of the 7th International Kimberlite Conference, Cape Town, South Africa, 1999 year: 1999 ident: 4001_CR33 contributor: fullname: R. H. Mitchell – ident: 4001_CR43 – volume: 12 start-page: 354 year: 2004 ident: 4001_CR39 publication-title: Petrologiya contributor: fullname: V. A. Pervov – volume: 76 start-page: 377 year: 2004 ident: 4001_CR15 publication-title: Lithos doi: 10.1016/j.lithos.2004.03.047 contributor: fullname: M. Heaman – start-page: 322 volume-title: Geology of Diamonds—Present and Future year: 2005 ident: 4001_CR27 contributor: fullname: V. A. Larchenko – ident: 4001_CR3 – volume: 268 start-page: 23 year: 1996 ident: 4001_CR34 publication-title: Tectonophysics doi: 10.1016/S0040-1951(96)00228-4 contributor: fullname: A. M. Nikishin – volume: 88 start-page: 267 year: 1985 ident: 4001_CR46 publication-title: Trans. Geol. Soc. South Africa contributor: fullname: C. B. Smith – volume-title: Carbonatites and Kimberlites (Relations, Metallogeny, and Forecasting) year: 2005 ident: 4001_CR11 contributor: fullname: A. A. Frolov – ident: 4001_CR36 – volume: 21 start-page: 22 year: 1999 ident: 4001_CR50 publication-title: Mineral. Zh. contributor: fullname: S. N. Tsymbal – volume: 21 start-page: 97 year: 1999 ident: 4001_CR51 publication-title: Mineral. Zh. contributor: fullname: S. N. Tsymbal – ident: 4001_CR28 – volume-title: Kimberlites, Orangeites and Related Rocks year: 1995 ident: 4001_CR32 doi: 10.1007/978-1-4615-1993-5 contributor: fullname: R. H. Mitchell – start-page: 625 volume-title: Proceedings of 7h International Kimberlite Conference, Cape Town, South Africa, 1999 year: 1999 ident: 4001_CR37 contributor: fullname: H. E. O’Brien – volume: 10 start-page: 493 year: 2002 ident: 4001_CR23 publication-title: Petrologiya contributor: fullname: V. A. Kononova – ident: 4001_CR21 – volume: 409 start-page: 662 year: 2006 ident: 4001_CR24 publication-title: Dokl. Akad. Nauk contributor: fullname: V. A. Kononova – volume: 402 start-page: 87 year: 2005 ident: 4001_CR56 publication-title: Dokl. Akad. Nauk contributor: fullname: E. V. Yutkina – start-page: 127 volume-title: Geochemistry of Magmatic Rocks year: 2005 ident: 4001_CR41 contributor: fullname: V. A. Pervov – ident: 4001_CR18 – volume: 386 start-page: 651 year: 2002 ident: 4001_CR8 publication-title: Dokl. Akad. Nauk contributor: fullname: N. A. Bozhko – ident: 4001_CR52 – volume: 38 start-page: 461 year: 1997 ident: 4001_CR17 publication-title: Geol. Geofiz. contributor: fullname: H. H. Helmstaedt |
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Snippet | Several episodes of kimberlite magmatism occurred in the East European Province (EEP) during a long (about 1.5 Gyr) time period, from the Late Paleoproterozoic... |
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SubjectTerms | Anomalies Biotite Composition Cratons Criteria Depletion Devonian Diamonds Distribution patterns Geochemistry Geology Kimberlites Lithosphere Magma Minerals Northern Hemisphere Ordovician Paleozoic Pattern recognition Petrology Platforms (geology) Rocks Titanium dioxide Trace elements Volatiles Zirconium |
Title | Kimberlites and lamproites of the East European Platform: Petrology and geochemistry |
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