Abstract
This research aims to reconstruct the Late Neoproterozoic-to-recent long-term time–temperature-evolution of the NW Namibian Kaoko and Damara belts combining numerical modeling of new thermochronological data with previously published geochronological data, i.e., U–Pb, Sm–Nd, and Rb–Sr analyses, and K/Ar, 40Ar/39Ar low-temperature thermochronology. Consequently, we retrieve a coherent long-term time–temperature-evolution of the NW Namibian Neoproterozoic basement rocks including rates of exhumation and subsidence periods over the last ~ 500 Myr. Neoproterozoic basement rocks indicate fast post-Pan African/Brasiliano cooling and exhumation, reheating, or rather subsidence during the development of the Paleozoic-to-Mesozoic SW Gondwana intraplate environment and a significant thermal overprint of the rocks during South Atlantic syn- to post-rift processes, and therefore, resemble the opponent SE Brazilian time–temperature-evolution. We provide an overview of thermochronological data including new apatite and zircon fission-track data derived from Neoproterozoic, Late Paleozoic, and Lower Cretaceous rocks. Apatite fission-track ages range from 390.9 ± 17.9 Ma to 80.8 ± 6.0 Ma in the NW Kaoko Belt with youngest ages confined to the coastal area and significant age increase towards the inland. New zircon apatite fission-track data reveal ages between 429.5 ± 47.8 and 313.9 ± 53.4 Ma for the rocks of the Kaoko Belt. In the central Damara Belt, new apatite fission-track ages range between 138.5 ± 25.3 Ma to 63.8 ± 4.8 Ma. Combined apatite fission-track age distributions from Angola to Namibia and SE Brazil correlate for both sides of the South Atlantic passive continental margin and the reset AFT ages overlap with the lateral Paraná–Etendeka dike swarm distribution.
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References
Baksi AK (2018) Paraná flood basalt volcanism primarily limiteds to ~1 Myr beginning at 135 Ma: new 40Ar/39Ar ages for rocks from Rio Grande do Sul, and critical evaluation of published radiometric data. J Volcanol Geoth Res 355:66–77. https://doi.org/10.1016/j.jvolgeores.2017.02.016
Barker CE, Pawlewicz MJ (1986) The correlation of vitrinite reflectance with maximum temperature in humic organic matter. In: Buntebarth G, Stegena L (eds) Paleogeothermics. Springer, Berlin, pp 79–93
Braun J (2018) A review of numerical modeling studies of passive margin escarpments leading to a new analytical expression for the rate of escarpment migration velocity. Gondwana Res 53:209–224. https://doi.org/10.1016/j.gr.2017.04.012
Brown RW, Rust DJ, Summerfield MA, Gleadow AJW, de Wit MCJ (1990) An early Cretaceous phase of accelerated erosion on the south-western margin of Africa: evidence from apatite fission track analysis and the offshore sedimentary record. Nucl Tracks Radiat Meas 17:339–350. https://doi.org/10.1016/1359-0189(90)90056-4
Brown R, Summerfield MA, Gleadow AJW, Gallagher K, Carter A, Beucher R, Wildman M (2014) Intracontinental deformation in southern Africa during the Late Cretaceous. J Afr Earth Sci 100:20–41. https://doi.org/10.1016/j.jafrearsci.2014.05.014
Bühn B, Häussinger H, Kramm U, Kukla C, Kukla PA (1994) Tectonometamorphic patterns developed during Pan-African continental collision in the Damara inland Belt, Namibia. Chem Erde 54:1–25
Burov E (2009) Thermo-mechanical models for coupled lithosphere-surface processes: applications to continental convergence and mountain building processes. In: Cloetingh S, Negendank J (eds) New Frontiers in integrated solid earth sciences. International year of planet earth. Springer, Dordrecht, pp 103–143. https://doi.org/10.1007/978-90-481-2737-5_4
Catuneanu O, Wopfner H, Eriksson PG, Cairncross B, Rubidge BS, Smith RMH, Hancox PJ (2005) The Karoo basins of south-central Africa. J Afr Earth Sci 43:211–253. https://doi.org/10.1016/j.jafrearsci.2005.07.007
Courtillot V, Jaupart C, Manighetti I, Tapponnier P, Besse J (1999) On causal links between flood basalts and continental breakup. Earth Planet Sci Lett 166:177–195. https://doi.org/10.1016/S0012-821X(98)00282-9
Donelinck R, Ketcham RA, Carlson WD (1999) Variability of fission-track annealing kinetics: II Crystallographic orientation effects. Am Mineral 84:1224–1234. https://doi.org/10.2138/am-1999-0902
Duncan RA, Hooper PR, Rehacek J, Marsh JS, Duncan AR (1997) The timing and duration of the Karoo igneous event, southern Gondwana. J Geophys Res 102:18127–18138. https://doi.org/10.1029/97JB00972
Engelmann de Oliveira CH, Jelinek AR, Chemale F Jr, Bernet M (2016a) Evidence of post-Gondwana breakup in Southern Brazilian shield: insights from apatite and zircon fission track thermochronology. Tectonophysics 666:173–187. https://doi.org/10.1016/j.tecto.2015.11.005
Engelmann de Oliveira CH, Jelinek AR, Chemale F Jr, Cupertino JA (2016b) Thermotectonic history of the southeastern Brazilian margin: evidence from apatite fission track data of the offshore Santos Basin and continental basement. Tectonophysics 685:21–34. https://doi.org/10.1016/j.tecto.2016.07.012
Ernst RE, Buchan KL (2001) Mantle plumes: their identification through time. Geol Soc Am Spec Pap 352:593
Florisbal LM, Heaman LM, de Assis JV, Bitencourt MF (2014) Tectonic significance of the Florianópolis dyke Swarm, Paraná–Etendeka magmatic province: a reappraisal based on precise U–Pb dating. J Volcanol Geoth Res 289:140–150. https://doi.org/10.1016/j.jvolgeores.2014.11.007
Foster DA, Goscombe BD, Gray DR (2009) Rapid exhumation of deep crust in an obliquely convergent orogeny: the Kaoko Belt of the Damara Orogen. Tectonics 28(TC4002):24. https://doi.org/10.1029/2008TC002317
Franco-Magalhães AOB, Hackspacher PC, Glasmacher UA, Saad AR (2010) Rift to post-rift evolution of a “passive” continental margin: the Ponta Grossa Arch, SE Brazil. Int J Earth Sci (Geologische Rundschau) 99:1599–1613. https://doi.org/10.1007/s00531-010-0556-8
Franke D (2013) Rifting, lithosphere breakup and volcanism: comparison of magma-poor and volcanic rifted margins. Mar Pet Geol 43:63–87. https://doi.org/10.1016/j.marpetgeo.2012.11.003
Frimmel HE, Frank W (1998) Neoproterozoic tectono-thermal evolution of the Gariep Belt and its basement, Namibia and South Africa. Precambr Res 90:1–28. https://doi.org/10.1016/S0301-9268(98)00029-1
Frimmel HE, Basei MS, Gaucher C (2011) Neoproterozoic geodynamic evolution of SW-Gondwana: a southern African perspective. Int J Earth Sci (Geologische Rundschau) 100:323–354. https://doi.org/10.1007/s00531-010-0571-9
Galbraith RF (1981) On statistical models for fission-track counts. Math Geol 13:471–478. https://doi.org/10.1007/BF01034498
Gallager K, Brown R (1997) The onshore record of passive margin evolution. J Geol Soc Lond 154:451–457. https://doi.org/10.1144/gsjgs.154.3.0451
Gallagher K, Hawkesworth CJ, Mantovani MSM (1994) The denudation history of the offshore continental margin of SE Brazil inferred from apatite fission-track data. J Geophys Res 99:18117–18145. https://doi.org/10.1029/94JB00661
Gallagher K, Hawkesworth CJ, Mantovani MSM (1995) Denudation, fission track analysis and the long-term evolution of passive margin topography: application to the southeast Brazilian margin. J S Am Earth Sci 8:65–77. https://doi.org/10.1016/0895-9811(94)00042-Z
Gallagher K, Brown R, Johnson C (1998) Fission track analysis and its applications to geological problems. Annu Rev Earth Planet Sci 26:519–572. https://doi.org/10.1146/annurev.earth.26.1.519
Garver JI (2003). Discussion: “Metamictization of natural zircon: accumulation versus thermal annealing of radioactivity-induced damage”. by Nasdala et al. (2001) Contributions to Mineralogy and Petrology 143:756–757. https://doi.org/10.1007/10.1007/s00410-002-0379-0
Garver JI, Kamp PJJ (2002) Integration of zircon color and zircon fission track zonation patterns in Orogenic belts: application of the Southern Alps, New Zealand. Tectonophysics 349:203–219. https://doi.org/10.1016/S0040-1951(02)00054-9
Gibson SA, Thompson RN, Day JA (2006) Timescales and mechanism of plume-lithosphere interactions: 40Ar/39Ar geochronology and geochemistry of alkaline igneous rocks from the Paraná–Etendeka large igneous province. Earth Planet Sci Lett 251:1–17. https://doi.org/10.1016/j.epsl.2006.08.004
Gleadow AJW (1981) Fission-track dating methods: What are the real alternatives? Nuclear Tracks 5:3–14. https://doi.org/10.1016/0191-278X(81)90021-4
Goscombe BD, Gray DR (2007) The coastal Terrane of the Kaoko Belt, Namibia: outboard arc-terrane and tectonic significance. Precambr Res 155:139–158. https://doi.org/10.1016/j.precamres.2007.01.008
Goscombe BD, Gray DR (2008) Structure and strain variation at mid-crustal levels in a transpressional orogeny: a review of Kaoko belt structure and the character of West Gondwana amalgamation and dispersal. Gondwana Res 12:45–85. https://doi.org/10.1016/j.gr.2007.07.002
Goscombe BD, Hand M, Gray DR (2003a) Structure of the Kaoko Belt, Namibia: progressive evolution of a classic transpressional orogen. J Struct Geol 25:1049–1081. https://doi.org/10.1016/S0191-8141(02)00150-5
Goscombe BD, Hand M, Gray DR, Mawby J (2003b) The metamorphic architecture of a transpressional orogen: the Kaoko Belt, Namibia. J Petrol 44:679–711. https://doi.org/10.1093/petrology/44.4.679
Goscombe BD, Gray DR, Armstrong RA, Foster DA, Vogl J (2005a) Event geochronology of the Pan-African Kaoko Belt, Namibia. Precambr Res 140:1–41. https://doi.org/10.1016/j.precamres.2005.07.003
Goscombe BD, Gray DR, Hand M (2005b) Extrusional tectonics in the core of a transpressional orogen, the Kaoko Belt, Namibia. J Petrol 46:1203–1241. https://doi.org/10.1093/petrology/egi014
Goscombe BD, Gray DR, Hand M (2006) Crustal architecture of the himalayan metamorphic front in eastern Nepal. Gondwana Res 10:232–255. https://doi.org/10.1016/j.gr.2006.05.003
Goscombe BD, Foster DA, Gray DR, Wade B (2017) Metamorphic response and crustal architecture in a classic collisional orogeny: the Damara Belt, Namibia. Gondwana Res 52:80–124. https://doi.org/10.1016/j.gr.2017.07.006
Gray DR, Foster DA, Goscombe BD, Passchier CW, Trouw RAJ (2006) 40Ar/39Ar thermochronology of the Pan-African Damara Orogen, Namibia, with implications for tectono-thermal and geodynamic evolution. Precambr Res 150:49–72. https://doi.org/10.1016/j.precamres.2006.07.003
Green PF (1986) On the thermo-tectonic evolution of Northern England: evidence from fission track analysis. Geol Mag 123:493–506. https://doi.org/10.1017/S0016756800035081
Green PF, Machado V (2015) Pre-rift and syn-rift exhumation, post-rift subsidence and exhumation of the onshore Namibe Margin of Angola revealed from apatite fission track analysis. Geol Soc Lond Spec Publ 438:99–118. https://doi.org/10.1144/SP438.2
Green PF, Duddy IR, Laslett GM, Hegarty KA, Gleadow AJW, Lovering JF (1998) Thermal annealing of fission tracks in apatite. 4. Quantitative modelling techniques and extension to geological timescales. Chem Geol (Isotope Geosci Sect) 79:155–182. https://doi.org/10.1016/0168-9622(89)90018-3
Green PF, Japsen P, Chalmers JA, Bonow JM, Duddy IR (2018) Post-breakup burial and exhumation of passive continental margins: seven propositions to inform geodynamic models. Gondwana Res 53:58–81. https://doi.org/10.1016/j.gr.2017.03.007
Guedes E, Heilbron M, Valeriano CM, Almeida JCH, Szatmari P (2016) Evidence of Gondwana early rifting process recorded by Resende-Ilha Grande Dike Swarm, southern Rio de Janeiro, Brazil. J S Am Earth Sci 67:11–24. https://doi.org/10.1016/j.jsames.2016.01.004
Haack U, Martin H (1983). Geochronology of the Damara Orogen—a review. In: Martin H, Eder FW (eds) Intracontinental fold belts. Springer, Berlin, pp 839–846. https://doi.org/10.1007/978-3-642-69124-9_36
Hartmann LA, Lopes WR, Savian JF (2016) Integrated evaluation of the geology, aerogammaspectrometry and aeromagnetometry of the Sul-Riograndense Shield, southernmost Brazil. Anais da Academia Brasileira de Ciencias 88:75–92. https://doi.org/10.1590/0001-3765201520140495
Heilbron M, Valeriano CM, Tassinari CCG, Almeida JCH, Tupinamba M, Siga O, Trouw RAJ (2008) Correlation of Neoproterozoic terranes between the Ribeira Belt, SE Brazil and its African counterpart: comparative tectonic evolution and open questions. Geol Soc Lond Spec Publ 294:211–237. https://doi.org/10.1144/SP294.12
Hiruma ST, Riccomini C, Modenesi-Gauttieri MC, Hackspacher PC, Neto JCH, Franco-Magalhaes AOB (2010) Denudation history of the Bocaina Plateau, Serra do Mar, south-eastern Brazil: relationships to Gondwana break-up and passive margin development. Gondwana Res 18:674–687. https://doi.org/10.1016/j.gr.2010.03.001
Hoffman PF, Kaufman AJ, Halverson GP, Schrag DP (1998) A Neoproterozoic snowball earth. Science 281:1342–1346. https://doi.org/10.1126/science.281.5381.1342
Hoffmann KH, Condon DJ, Bowring SA, Crowley JL (2004) U-Pb zircon date from the Neoproterozoic Ghaub Formation, Namibia: constraints on Marinoan glaciation. Geology 32(9):817
Hu J, Liu L, Faccenda M, Zhou Q, Fischer KM, Marshak S, Lundstrom C (2018) Modification of the Western Gondwana craton by plume-lithosphere interaction. Nat Geosci 11:203–210. https://doi.org/10.1038/s41561-018-0064-1
Hurford AJ (1986) Standardization of fission-track dating calibration: results of questionnaire distributed by International Union of Geosciences Sub commission on geochronology. Nucl Tracks 11:329–333. https://doi.org/10.1016/1359-0189(86)90061-0
Jackson MPA, Cramez C, Fonck JM (2000) Role of subaerial volcanic rocks and mantle plumes in creation of South Atlantic margins: implications for salt tectonics and source rocks. Mar Pet Geol 17:477–498. https://doi.org/10.1016/S0264-8172(00)00006-4
Japsen P, Bonow JM, Green PF, Cobbold PR, Chiossi D, Lilletveit R, Magnavita LP, Pedreira A (2012) Episodic burial and exhumation in BE Brazil after opening of the South Atlantic. Geol Soc Am Bull 124:800–816. https://doi.org/10.1130/B30515.1
Japsen P, Green PF, Bonow JM, Nielsen TFD, Chalmers JA (2014) From volcanic plains to glaciated peaks: burial, uplift and exhumation history of Southern East Greenland after opening of the NE Atlantic. Glob Planet Change 116:91–114. https://doi.org/10.1016/j.gloplacha.2014.01.012
Jelinek AR, Chemale F Jr, van der Beek PA, Guadagnin F, Cupertino JA, Viana A (2014) Denudation history and landscape evolution of the northern East-Brazilian continental margin from apatite fission-track thermochronology. J S Am Earth Sci 54:158–181. https://doi.org/10.1016/j.jsames.2014.06.001
Jerram D, Moutney N, Holzförster F, Stollhofen H (1999) Internal stratigraphic relationships in the Etendeka group in the Huab Basin, NW Namibia: understanding the onset of flood volcanism. J Geodyn 28:393–418. https://doi.org/10.1016/S0264-3707(99)00018-6
Johnson MR, Van Vuuren CJ, Hegenberger WF, Key R, Shoko U (1996) Stratigraphy of the Karoo Supergroup in southern Africa: an overview. J Afr Earth Sc 23:3–15. https://doi.org/10.1016/S0899-5362(96)00048-6
Jung S, Mezger K (2001) Geochronology in migmatites—a Sm-Nd, U-Pb, and Rb-Sr study from the Proterozoic Damara belt (Namibia): implications for polyphase development of migmatites in high-grade terranes. J Metamorph Geol 19:77–97. https://doi.org/10.1046/j.0263-4929.2000.00297.x
Jung S, Hoernes S, Mezger K (2000a) Geochronology and petrogenesis of Pan African syn-tectonic S-type and post-tectonic A-type granite (Namibia)—products of melting of crustal sources, fractional crystallization and wall rock entrainment. Lithos 50:259–287. https://doi.org/10.1016/S0024-4937(99)00059-6
Jung S, Hoernes S, Mezger K (2000b) Geochronology and petrology of migmatites from the Proterozoic Damara Belt—importance of episodic fluid-present disequilibrium melting and consequences for granite petrology. Lithos 51:153–179. https://doi.org/10.1016/S0024-4937(99)00062-6
Jung S, Brandt S, Nebel O, Hellebrand E, Seth B, Jung C (2014) The P-T-t paths of high-grade gneisses, Kaoko Belt, Namibia: constraints from mineral data, U–Pb allanite and monazite and Sm-Nd/Lu-Hf garnet ages and garnet ion probe data. Gondwana Res 25:775–796. https://doi.org/10.1016/j.gr.2013.05.017
Karl M, Glasmacher UA, Kollenz S, Franco-Magalhaes AOB, Stockli DF, Hackspacher PC (2013) Evolution of the South Atlantic passive continental margin in southern Brazil derived from zircon and apatite (U–Th–Sm)/He and fission-track data. Tectonophysics 604:224–244. https://doi.org/10.1016/j.tecto.2013.06.017
Ketcham RA (2005) Forward and Inverse Modelling of low-temperature thermochronometry data. Rev Mineral Geochem 58:275–314. https://doi.org/10.2138/rmg.2005.58.11
Ketcham RA (2017) HeFTy version 1.9.3, Manual
Ketcham RA, Carter A, Donelick RA, Barbarand J, Hurford AJ (2007a) Improved measurements of fission-track annealing in apatite using c-axis projection. Am Miner 92:789–798. https://doi.org/10.2138/am.2007.2280
Ketcham RA, Carter A, Donelick RA, Barbarand J, Hurford AJ (2007b) Improved modelling of fission-track annealing in apatite. Am Miner 92:799–810. https://doi.org/10.2138/am.2007.2281
Ketcham RA, Donelick RA, Balestrieri ML, Zattin M (2009) Reproducibility of apatite fission-track length data and thermal history reconstruction. Earth Planet Sci Lett 284:504–515. https://doi.org/10.1016/j.epsl.2009.05.015
Konopásek J, Kosler J, Tajcmanove L, Ulrich S, Kitt SL (2008) Neoproterozoic igneous complex emplaced along major tectonic boundary in the Kaoko Belt (NW Namibia): ion probe and LA-ICP-MS dating of magmatic and metamorphic zircons. J Geol Soc Lond 165:153–165. https://doi.org/10.1144/0016-76492006-192
Krob FC, Glasmacher UA, Karl M, Perner M, Hackspacher PC, Stockli DF (2019) Multi-chronometer thermochronological modelling of the Late Neoproterozoic to recent t–T-evolution of the SE coastal region of Brazil. J S Am Earth Sci 92:77–94. https://doi.org/10.1016/j.jsames.2019.02.012
Kröner S, Konopásek J, Kröner A, Passchier CW (2004) U–Pb and Pb–Pb zircon ages for metamorphic rocks in the Kaoko belt of Northwestern Namibia: a Palaeo- to Mesoproterozoic basement reworked during the Pan-African orogeny. S Afr J Geol 107:455–476. https://doi.org/10.2113/107.3.455
Kröner S, Rojas-Agramonte Y, Hegner E, Hoffmann K-H, Wingate MTD (2010) SHRIMP zircon dating and Nd isotopic systematics of Palaeoproterozoic migmatitic orthogneisses in the Epupa Metamorphic Complex of northwestern Namibia. Precambr Res 183:50–69. https://doi.org/10.1016/j.precamres.2010.06.018
Kukla C (1993) Strontium isotope heterogeneities in amphibolite facies, banded metasediments: a case study from the Late Proterozoic Kuiseb formation of the Southern Damara orogen, Central Namibia. Commun Geol Surv Namib Mem 15:139
Kukla C, Kramm U, Kukla PA, Okrusch M (1991) U-Pb monazite data relating to metamorphism and granite intrusion in the northwestern Khomas Trough, Damara Orogen, central Namibia. Commun Geol Surv Namib 7:49–54
Kukulus M (2004) A quantitative approach to the evolution of the Walvis Basin offshore NW-Namibia: structure, mass balancing, and hydrocarbon potential. Dissertation, Julius-Maximilians-Universität Würzburg, Germany.
Lewis CLE, Green PF, Carter A, Hurford AJ (1992) Elevated K/T palaeotemperatures throughout Northwest England: three kilometers of Tertiary erosion? Earth Planet Sci Lett 112:131–145. https://doi.org/10.1016/0012-821X(92)90012-K
Lobo-Guerrero Sanz A (2005) Pre- and Post-Katangan Granitoids of the greater Lufilian Arc—geology, geochemistry, geochronology and metallogenic significance. Dissertation, University of the Witwatersrand, Johannesburg, South Africa
Marzioli A, Melluso VM, Renne PR, Sgrosso I, D’Antonio M, Morais LD, Morais EAA, Ricci G (1999) Geochronology and petrology of Cretaceous basaltic magmatism in the Kwanza basin (western Angola), and relationships with the Paraná–Etendeka continental flood basalt province. J Geodyn 28:341–356. https://doi.org/10.1016/S0264-3707(99)00014-9
Milani EJ, de Melo JHG, de Souza PA, Fernandes LA, França AB (2007) Bacia do Paraná. Boletim de Geociěncias - Petrobras, Rio de Janeiro 15:265–287
Milani L, Kinnaird JA, Lehmann J, Naydenov KV, Saalmann K, Frei D, Gerdes A (2015) Role of crustal contribution in the early stage of the Damara Orogen, Namibia: new constraints from combined U–Pb and Lu–Hf isotopes from the Goas Magmatic complex. Gondwana Res 28:961–986. https://doi.org/10.1016/j.gr.2014.08.007
Miller RMG (1983) The Pan-African Damara orogen of Namibia. In: Miller RMG (ed) Evolution of the Damara Orogen of South West Africa/Namibia. Spec Publ Geol Soc S Afr 11:431–515.
Miller RMG (2008) Neoproterozoic and early Palaeozoic rocks of the Damara Orogen. In: Miller RM (ed) The geology of Namibia. Geological Survey of Namibia, Windhoek
Miller RMG (2013) Comparative stratigraphic and geochronological evolution of the Northern Damara Supergroup in Namibia and the Katanga Supergroup in the Lufilian Arc of Central Africa. Geosci Can 40(2):118
Miller RMG, Burger AJ (1983) U-Pb zircon ages of members of the Salem Granitic Suite along the northern edge of the central Damara granite belt. In: Miller RMG (ed) Evolution of the Damara Orogen of South West Africa/Namibia. Spec Publ Geol Soc South Afr 11:273–280
Milner SC (1986) The geological and volcanological features of the quartz latites of the Etendeka formation. Commun Geol Surv Southwest Africa/Namibia 2:109–116
Milner SC, Duncan AR, Ewart A (1992) Quartz latite rheoignimbrite flows of the Etendeka Formation, north-western Namibia. Bull Volcanol 54:200–219. https://doi.org/10.1007/BF00278389
Milner SC, Le Roex AP, O’Conner JM (1995) Age of Mesozoic igneous rocks in northwestern Namibia, and their relationship to continental breakup. J Geol Soc 152:97–104. https://doi.org/10.1144/gsjgs.152.1.0097
Montañez IP, Poulsen CJ (2013) The late Paleozoic ice age: an evolving paradigm. Annu Rev Earth Planet Sci 41:629–656. https://doi.org/10.1146/annurev.earth.031208.100118
Nascimento DB, Ribeiro A, Trouw RAJ, Schmitt RS, Passchier CW (2016) Stratigraphy of the Neoproterozoic Damara Sequence in northwest Namibia: slope to basin sub-marine mass-transport deposits and olistolith fields. Precambr Res 278:108–125. https://doi.org/10.1016/j.precamres.2016.03.005
Oyhantcabal P, Siegesmund S, Wemmer K, Passchier CW (2011) The transpressional connection between Dom Feliciano and Kaoko Belt at 580–550 Ma. Int J Earth Sci (Geologische Rundschau) 100:379–390. https://doi.org/10.1007/s00531-010-0577-3
Peate DW (1997) The Paraná–Etendeka Province. In: Mahoney JJ, Coffin MF (eds) Large Igneous Provinces: continental, oceanic, and planetary flood volcanism. Geophysical Monograph 100. Washington, DC: American Geophysical Union, pp 217–245.
Pollard S (2002) Temperature range of thermochronometers: temperatures that are in current use, and their effective closure temperatures (adapted from Fitzgerald P, Baldwin S, Gehrels G, Reiners P, Ducea M). https://pangea.standard.edu/~dpollard/NSF/main.html.
Raab MJ (2001) The geomorphic response of the passive continental margin of Northern Namibia to Gondwana break-up and global scale tectonics. Dissertation. Georg-August-University, Göttingen, Germany
Raab MJ, Brown RW, Gallagher K, Carter A, Weber K (2002) Late Cretaceous reactivation of major crustal shear zones in northern Namibia: constraints from apatite fission track analysis. Tectonophysics 349:75–92. https://doi.org/10.1016/S0040-1951(02)00047-1
Raab MJ, Brown RW, Gallagher K, Weber K, Gleadow AJW (2005) Denudational and thermal history of the Early cretaceous Brandberg and Kenyenya igneous complexes on Namibia’s Atlantic passive margin. Tectonics 24(TC3006):15. https://doi.org/10.1029/2004TC001688
Rahn MK, Brandon MT, Batt GE, Garver JI (2004) A zero-damage model for fission-track annealing in zircon. Am Miner 89:473–484. https://doi.org/10.2138/am-2004-0401
Reiners PW, Brandon MT (2006) Using thermochronology to understand orogenetic erosion. Annu Rev Earth Planet Sci 34:419–466. https://doi.org/10.1146/annurev.earth.34.031405.125202
Renne PR, Deckart K, Ernesto M, Féraud G, Piccirillo EM (1996) Age of Ponta Grossa dike swarm (Brazil), and implications to Parana flood volcanism. Earth Planet Sci Lett 144:199–221. https://doi.org/10.1016/0012-821X(96)00155-0
Rybach L (1988) Determination of heat production rate. In: Haenel R, Rybach L, Stegena L (eds) Handbook of terrestrial heat flow density determination. Kluwer Academic Publishers, Dordrecht, pp 125–142
Salomon E, Koehn D, Passchier CW (2015) Brittle reactivation of ductile shear zones in NW Namibia in relation to South Atlantic rifting. Tectonics 34:70–85. https://doi.org/10.1002/2014TC003728
Salomon E, Koehn D, Passchier CW, Chung P, Häger T, Salvona A, Davis J (2016) Deformation and fluid flow in the Huab Basin and Etendeka Plateau, NW Namibia. J Struct Geol 88:46–62. https://doi.org/10.1016/j.jsg.2016.05.001
Salomon E, Passchier CW, Koehn D (2017) Asymmetric continental deformation during South Atlantic rifting along southern Brazil and Namibia. Gondwana Res 51:170–176. https://doi.org/10.1016/j.gr.2017.08.001
Schmitt RS, Trouw RAJ, Passchier CW, Medeiros SR, Armstrong R (2012) 530 Ma syntectonic and granites in NW Namibia—their relation with collision along the junction of the Damara and Kaoko belts. Gondwana Res 21:362–377. https://doi.org/10.1016/j.gr.2011.08.006
Scotese CR, Golonka J (1992) PALEOMAP paleogeographic atlas. PALEOMAP Progress Report 20, Department of Geology, University of Texas, Arlington, Texas, p 34
Scotese CR, Boucot AJ, McKerrow WS (1999) Gondwanan paleogeography and paleoclimatology. J Afr Earth Sc 28:99–114. https://doi.org/10.1016/S0899-5362(98)00084-0
Şengör AMC (2001) Elevation as indicator of mantle-plume activity. In: Ernst RE, Buchan KL (eds) Mantle plumes: their identification through time. Geol Soc Am Spec Pap 352:183–225
Seth B, Kröner A, Mezger K, Nemchin AA, Pidgeon RT, Okrusch M (1998) Archaean to Neoproterozoic magmatic events in the Kaoko belt of NW Namibia and their geodynamic significance. Precambr Res 92:341–363. https://doi.org/10.1016/S0301-9268(98)00086-2
Seth B, Okrusch M, Wilde M, Hoffmann KH (2000) The Voetspoor Intrusion, Southern Kaoko Zone, Namibia: mineralogical, geochemical and isotopic constraints for the origin of a syenitic magma. Commun Geol Surv Namib 12:143–156
Silva BV, Hackspacher PC, Ribeiro MCS, Glasmacher UA, Gonçalves AO, Doranti-Tiritan C, Godoy DF, Constantino RR (2019) Evolution of the Southwestern Angolan Margin: episodic burial and exhumation is more realistic than long-term denudation. Int J Earth Sci (Geologische Rundschau) 108:89–113. https://doi.org/10.1007/s00531-018-1644-4
Stanistreet IG, Kukla PA, Henry G (1991) Sedimentary basinal responses to Late Precambrian Wilson cycles; the Damara Orogen and Nama Foreland, Namibia. J Afr Earth Sc 13:141–156. https://doi.org/10.1016/0899-5362(91)90048-4
Stollhofen H (1999) Karoo Synrift-Sedimentation und ihre tektonische Kontrolle am entstehenden Kontinentalrand Namibia. Zeitschrift der deutschen geologischen Gesellschaft 149:519–632
Stollhofen H, Stanisstreet IG, Bangert B, Grill H (2000) Tuffs, tectonism and glacially related sea-level changes, Carboniferous-Permian, southern Namibia. Palaeogeogr Palaeoclimatol Palaeoecol 161:127–150. https://doi.org/10.1016/S0031-0182(00)00120-6
Tello Saenz CA, Hackspacher PC, Hadler Neto JC, Lunes PJ, Guedes S, Ribeiro LFB, Paulo SR (2003) Recognition of Cretaceous, Paleocene, and Neogene tectonic reactivation through apatite fission-track analysis in Precambrian areas of southeast Brazil: association with the opening of the south Atlantic Ocean. J S Am Earth Sci 15:765–774. https://doi.org/10.1016/S0895-9811(02)00131-1
Thompson RN, Gibson SA, Dicking AP, Smith PM (2001) Early Cretaceous Basalt and Picrite dykes of the Southern Etendeka Region, NW Namibia: windows into the role of the Tristan Mantle plume in Paraná–Etendeka magmatism. J Petrol 42:2049–2081. https://doi.org/10.1093/petrology/42.11.2049
Torsvik TH, Rousse S, Labails C, Smethurst MA (2009) A new scheme for the opening of the South Atlantic ocean and the dissection of an Aptian salt basin. Geophys J Int 177:1315–1333. https://doi.org/10.1111/j.1365-246X.2009.04137.x
Torsvik TH, von der Voo R, Doubrovine PV, Burke K, Steinberger B, Ashwal LD, Trønnes RG, Webb SJ, Bull AL (2014) Deep mantle structures as a reference frame for movements in and on the Earth. Proc Natl Acad Sci USA 111:8735–8740. https://doi.org/10.1073/pnas.1318135111
Travassos RP (2014) Interpretação estrutural regional do escudo Sul-Rio-Grandense -Rio Grande do Sul, Brasil, com base em aeromagnetometria. Dissertation. Instituto de Geosciencias, Universidade de Brasilia, Brazil
Trumbull RB, Vietor T, Hahne K, Wackerle R, Ledru P (2004) Aeromagnetic mapping and reconnaissance geochemistry of the Early Cretaceous Henties Bay-Outjo dike swarm, Etendeka Igneous Province, Namibia. J Afr Earth Sc 40:17–29. https://doi.org/10.1016/j.jafrearsci.2004.07.006
Trumbull RB, Reid DL, de Beer C, van Acken D, Romer RL (2007) Magmatism and continental breakup at the west margin of southern Africa: a geochemical comparison of dolerite dikes from northwestern Namibia and the Western Cape. S Afr J Geol 110:477–502. https://doi.org/10.2113/gssajg.110.2-3.477
Uliana MA, Legarreta L, Laffitte GA, Villar HJ (2014) Estratigrafía y Geoquímica de la facies generadoras de hidrocarburos en la cuencas petrolíferas de Argentina. IV Congreso de Exploración y Desarrollo de Hidrocarburos (Mar del Plata). Actas 1:1–63
Van de Flierdt T, Hoernes S, Jung S, Masberg P, Hoffer E, Schaltegger U, Friedrichsen H (2003) Lower crustal melting and the role of open-system processes in the genesis of syn-orogenic quartz diorite–granite–leucogranite associations: constraints from Sr–Nd–O isotopes from the Bandombaai complex, Namibia. Lithos 67:205–226. https://doi.org/10.1016/S0024-4937(03)00016-1
Wilson JT (1963) A possible origin of the Hawaiian islands. Can J Phys 41:863–870. https://doi.org/10.1139/p63-094
Wilson JT (1965) A new class of faults and their bearing on continental drift. Nature 207:343–347. https://doi.org/10.1038/207343a0
Wygrala BP (1989) Integrated Study of an oil field in the southern Po Basin, northern Italy. KFA-Jülich 2313, 328 p. https://hdl.handle.net/2128/6740
Yalçin MN, Littke R, Sachsenhofer RF (1997) Thermal history of sedimentary basins. In: Welte DH, Horsfield B, Baker DR (eds) Petroleum and basin evolution. Springer, Berlin, pp 71–167. https://doi.org/10.1007/978-3-642-60423-2_3
Acknowledgements
Special thanks go to PhD Melissa Perner and dipl. geol. Markus Karl who did the field work during their stay at our research group. We also very much appreciate the discussions with members of the SPP-1375 SAMPLE. Furthermore, we like to thank Richard A. Ketcham and Raymond A. Donelick for providing the computer code HeFTy, Raymond A. Donelick allowing us to use Dpar® as a kinetic factor, and István Dunkl for providing the software code TrackKey. We would like to thank Prof. Dr. Paul Green, Prof. Dr. Peter Kukla, and two unknown reviewers for their critical reading and constructive comments on earlier versions of the manuscripts that led to significant improvements. In addition, we very much appreciate the technical support given by the Forschungs-Neutronenquelle FRM II at Garching, TU München, Germany organized by Dr. Gerstenberg.
Funding
Financial support provided with grants to Ulrich A. Glasmacher by the German Research Foundation (Deutsche Forschungsgemeinschaft, DFG, GL182/14-1, 14-2, GL 182/18-1) within the Priority Program 1375 (SAMPLE) and the DAAD (50753850) gratefully acknowledged.
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Krob, F.C., Eldracher, D.P., Glasmacher, U.A. et al. Late Neoproterozoic-to-recent long-term t–T-evolution of the Kaoko and Damara belts in NW Namibia. Int J Earth Sci (Geol Rundsch) 109, 537–567 (2020). https://doi.org/10.1007/s00531-020-01819-7
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DOI: https://doi.org/10.1007/s00531-020-01819-7