Abstract
Detrital thermochronology is based on the radiometric dating of apatite, zircon and other minerals in sediments and sedimentary rocks. The objective of detrital thermochronology is to obtain quantitative information on sediment provenance and on the geologic evolution of the area from whence the sediment was generated. This chapter describes how the full potential of the detrital thermochronology approach can be exploited by applying simple sedimentology principles, in order to obtain provenance information that is largely independent from the physical and chemical modifications affecting sediment during transport, deposition and burial diagenesis. Simple strategies can be used to detect the effects of selective entrainment, which form placer and antiplacer deposits, and test the vulnerability of grain-age distributions to hydraulic sorting effects. The mineral fertility of eroded bedrock, which varies over orders of magnitude thus representing the largest source of potential bias in detrital thermochronology, can be readily measured by simple modifications to the standard procedures of mineral concentration. Multi-method studies are potentially biased by grain rounding and abrasion, as the removal of grain rims may lead to an incorrect interpretation of grain ages yielded by low-temperature thermochronometers. Bedload and suspended load have different transport time, and the instantaneous-transport-time assumption of exhumation studies based on the lag-time approach is not necessarily met.
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References
Afanas’ ev VP, Nikolenko EI, Tychkov NS et al (2008) Mechanical abrasion of kimberlite indicator minerals: experimental investigations. Russ Geol Geophys 49(2):91–97
Allen PA, Allen JR (2013) Basin analysis: principles and application to petroleum play assessment. Wiley, New York
Andò S, Garzanti E, Padoan M, Limonta M (2012) Corrosion of heavy minerals during weathering and diagenesis: a catalogue for optical analysis. Sed Geol 280:165–178
Anfinson OA, Malusà MG, Ottria G, Dafov LN, Stockli DF (2016) Tracking coarse-grained gravity flows by LASS-ICP-MS depth-profiling of detrital zircon (Aveto Formation, Adriatic Foredeep, Italy). Mar Petrol Geol 77:1163–1176
Asti R, Malusà MG, Faccenna C (2018) Supradetachment basin evolution unraveled by detrital apatite fission track analysis: the Gediz Graben (Menderes Massif, Western Turkey). Basin Res 30:502-521
Baldwin SL (2015) Highlights and breakthroughs. Zircon dissolution and growth during metamorphism. Am Mineral 100(5–6):1019–1020
Bernet M, Zattin M, Garver JI, Brandon MT, Vance JA (2001) Steady-state exhumation of the European Alps. Geology 29:35–38
Bonich MB, Samson SD, Fedo CM (2017) Incongruity of detrital zircon ages of granitic bedrock and its derived alluvium: an example from the Stepladder Mountains, Southeastern California. J Geol 125(3)
Bramlette MN (1941) The stability of minerals in sandstone. J Sediment Res 11(1)
Carrapa B, Di Giulio A, Wijbrans J (2004) The early stages of the Alpine collision: an image derived from the upper Eocene–lower Oligocene record in the Alps-Apennines junction area. Sediment Geol 171:181–203
Carroll D (1953) Weatherability of zircon. J Sediment Res 23:106–116
Carter A, Moss SJ (1999) Combined detrital-zircon fission-track and U-Pb dating: a new approach to understanding hinterland evolution. Geology 27(3):235–238
Cavazza W, Gandolfi G (1992) Diagenetic processes along a basin-wide marker bed as a function of burial depth. J Sediment Res 62(2):261–272
Cawood PA, Nemchin AA, Freeman M, Sircombe K (2003) Linking source and sedimentary basin: detrital zircon record of sediment flux along a modern river system and implications for provenance studies. Earth Planet Sci Lett 210:259–268
Cheng NS (1997) Simplified settling velocity formula for sediment particle. J Hydraul Eng 123:149–152
Cheng NS (2009) Comparison of formulas for drag coefficient and settling velocity of spherical particles. Powder Tech 189:395–398
Cleary WJ, Conolly JR (1972) Embayed quartz grains in soils and their significance. J Sed Petr 42:899–904
Colin F, Alarcon C, Vieillard P (1993) Zircon: an immobile index in soils? Chem Geol 107:273–276
Corfu F, Hanchar JM, Hoskin PW, Kinny P (2003) Atlas of zircon textures. Rev Mineral Geochem 53(1):469–500
Dickinson WR (1985) Interpreting provenance relations from detrital modes of sandstones. Provenance of arenites. Springer, Netherlands, pp 333–361
Dickinson WR (2008) Impact of differential zircon fertility of granitoid basement rocks in North America on age populations of detrital zircons and implications for granite petrogenesis. Earth Planet Sci Lett 275:80–92
Dietz V (1973) Experiments on the influence of transport on shape and roundness of heavy minerals. Contrib Sediment 1:69–102
Doyle LJ, Carder KL, Steward RG (1983) The hydraulic equivalence of mica. J Sediment Res 53(2)
Dupré B, Gaillardet J, Rousseau D, Allègre CJ (1996) Major and trace elements of river-borne material: the Congo Basin. Geochim Cosmochim Ac 60:1301–1321
Eplett WJR (1982) The distributions of Smirnov type two-sample rank tests for discontinuous distributions functions. J Royal Stat Soc 44:361–369
Ewing RC, Meldrum A, Wang L, Weber WJ, Corrales LR (2003) Radiation effects in zircon. Rev Mineral Geochem 53:387–425
Fedele JJ, Paola C (2007) Similarity solutions for fluvial sediment fining by selective deposition. J Geophys Res-Earth 112:F02038
Fedo CM, Sircombe KN, Rainbird RH (2003) Detrital zircon analysis of the sedimentary record. Rev Mineral Geochem 53:277–303
Folk RL, Ward WC (1957) Brazos River bar: a study in the significance of grain size parameters. J Sediment Res 27:3–26
Garver JI, Kamp PJJ (2002) Integration of zircon color and zircon fission-track zonation patterns in orogenic belts: application to the Southern Alps, New Zealand. Tectonophysics 349:203–219
Garver JI, Brandon MT, Roden-Tice MK, Kamp PJJ (1999) Exhumation history of orogenic highlands determined by detrital fission track thermochronology. Geol Soc Spec Publ 154:283–304
Garzanti E, Andò S (2007) Heavy mineral concentration in modern sands: implications for provenance interpretation. Dev Sediment 58:517–545
Garzanti E, Malusà MG (2008) The Oligocene Alps: Domal unroofing and drainage development during early orogenic growth. Earth Planet Sci Lett 268:487–500
Garzanti E, Andò S, Vezzoli G (2008) Settling equivalence of detrital minerals and grain-size dependence of sediment composition. Earth Planet Sci Lett 273:138–151
Garzanti E, Andò S, Vezzoli G (2009) Grain-size dependence of sediment composition and environmental bias in provenance studies. Earth Planet Sci Lett 277:422–432
Garzanti E, Andò S, France-Lanord C, Censi P, Vignola P, Galy V, Lupker M (2010) Mineralogical and chemical variability of fluvial sediments: 1. Bedload sand (Ganga–Brahmaputra, Bangladesh). Earth Planet Sci Lett 299:368–381
Garzanti E, Padoan M, Andò S, Resentini A, Vezzoli G, Lustrino M (2013) Weathering and relative durability of detrital minerals in equatorial climate: sand petrology and geochemistry in the East African Rift. J Geol 121:547–580
Garzanti E, Resentini A, Andò S, Vezzoli G, Pereira A, Vermeesch P (2015) Physical controls on sand composition and relative durability of detrital minerals during long-distance littoral and eolian transport (coastal Namibia). Sedimentology 62:971–996
Gleadow AJW, Lovering JF (1974) The effect of weathering on fission track dating. Earth Planet Sci Lett 22(2):163–168
Glotzbach C, van der Beek P, Carcaillet J, Delunel R (2013) Deciphering the driving forces of erosion rates on millennial to million-year timescales in glacially impacted landscapes: an example from the Western Alps. J Geophys Res-Earth 118:1491–1515
Glotzbach C, Busschers FS, Winsemann J (2017) Detrital thermochronology of Rhine, Elbe and Meuse river sediment (Central Europe): implications for provenance, erosion and mineral fertility. Int J Earth Sci. https://doi.org/10.1007/s00531-017-1502-9
Graham SA, Dickinson WR, Ingersoll RV (1975) Himalayan-Bengal model for flysch dispersal in the Appalachian-Ouachita system. Geol Soc Am Bull 86:273–286
Granet M, Chabaux F, Stille P, Dosseto A, France-Lanord C, Blaes E (2010) U-series disequilibria in suspended river sediments and implication for sediment transfer time in alluvial plains: the case of the Himalayan rivers. Geochim Cosmochim Ac 74(10):2851–2865
Hay DC, Dempster TJ (2009) Zircon alteration, formation and preservation in sandstones. Sedimentology 56(7):2175–2191
He M, Zheng H, Bookhagen B, Clift P (2014) Controls on erosion intensity in the Yangtze River basin tracked by U-Pb detrital zircon dating. Earth-Sci Rev 136:121–140
Hietpas J, Samson S, Moecher D, Chakraborty S (2011) Enhancing tectonic and provenance information from detrital zircon studies: assessing terrane-scale sampling and grain-scale characterization. J Geol Soc London 168:309–318
Hodges KV, Ruhl KW, Wobus CW, Pringle MS (2005) 40Ar/39Ar thermochronology of detrital minerals. Rev Mineral Geochem 58:239–257
Hollander M, Wolfe D (1999) Nonparametric statistical methods. Wiley, New York
Horbe AMC, Horbe MA, Suguio K (2004) Tropical spodosols in northeastern Amazonas State, Brazil. Geoderma 119:55–68
Hourigan JK, Reiners PW, Brandon MT (2005) U-Th zonation-dependent alpha-ejection in (U-Th)/He chronometry. Geochim Cosmochim Ac 69:3349–3365
Hubert JF (1962) A zircon-tourmaline-rutile maturity index and the interdependence of the composition of heavy mineral assemblages with the gross composition and texture of sandstones. J Sediment Res 32:440–450
Ingersoll RV, Dickinson WR, Graham SA (2003) Remnant-ocean submarine fans: largest sedimentary systems on Earth. Geol S Am S 370:191–208
Johnsson MJ (1993) The system controlling the composition of clastic sediments. Geol S Am S 284:1–20
Jourdan S, Bernet M, Tricart P, Hardwick E, Paquette JL, Guillot S, Dumont T, Schwartz S (2013) Short-lived, fast erosional exhumation of the internal western Alps during the late early Oligocene: constraints from geothermochronology of pro-and retro-side foreland basin sediments. Lithosphere 5(2):211–225
Kohn MJ, Corrie SL, Markley C (2015) The fall and rise of metamorphic zircon. Am Mineral 100(4):897–908
Kohn B, Chung L, Gleadow A (2018) Chapter 2. Fission-track analysis: field collection, sample preparation and data acquisition. In: Malusà MG, Fitzgerald PG (eds) Fission-track thermochronology and its application to geology. Springer, Berlin
Komar PD (2007) The entrainment, transport and sorting of heavy minerals by waves and currents. Dev Sediment 58:3–48
Komar PD, Li Z (1988) Applications of grain-pivoting and sliding analyses to selective entrapment of gravel and to flow-competence evaluations. Sedimentology 35:681–695
Komar PD, Wang C (1984) Processes of selective grain transport and the formation of placers on beaches. J Geol 92:637–655
Kuenen PH (1959) Experimental abrasion; 3, fluviatile action on sand. Am J Sci 257:172–190
Kuenen PH (1960) Experimental abrasion 4: eolian action. J Geol 68:427–449
Lång LO (2000) Heavy mineral weathering under acidic soil conditions. Appl Geochem 15(4):415–423
Le Roux JP (2005) Grains in motion: a review. Sediment Geol 178:285–313
Le Roux G, Laverret E, Shotyk W (2006) Fate of calcite, apatite and feldspars in an ombrotrophic peat bog, Black Forest. Germany. J Geol Soc London 163(4):641–646
Malusà MG (2018) Chapter 16. A guide for interpreting complex detrital age patterns in stratigraphic sequences. In: Malusà MG, Fitzgerald PG (eds) Fission-track thermochronology and its application to geology. Springer, Berlin
Malusà MG, Fitzgerald PG (2018) Chapter 8. From cooling to exhumation: setting the reference frame for the interpretation of thermocronologic data. In: Malusà MG, Fitzgerald PG (eds) Fission-track thermochronology and its application to geology. Springer, Berlin
Malusà MG, Fitzgerald PG (2018) Chapter 10. Application of thermochronology to geologic problems: bedrock and detrital approaches. In: Malusà MG, Fitzgerald PG (eds) Fission-track thermochronology and its application to geology. Springer, Berlin
Malusà MG, Zattin M, Andò S, Garzanti E, Vezzoli G (2009) Focused erosion in the Alps constrained by fission-track ages on detrital apatites. Geol Soc Spec Publ 324:141–152
Malusà MG, Villa IM, Vezzoli G, Garzanti E (2011) Detrital geochronology of unroofing magmatic complexes and the slow erosion of Oligocene volcanoes in the Alps. Earth Planet Sci Lett 301(1):324–336
Malusà MG, Carter A, Limoncelli M, Villa IM, Garzanti E (2013) Bias in detrital zircon geochronology and thermochronometry. Chem Geol 359:90–107
Malusà MG, Resentini A, Garzanti E (2016a) Hydraulic sorting and mineral fertility bias in detrital geochronology. Gondwana Res 31:1–19
Malusà MG, Anfinson OA, Dafov LN, Stockli DF (2016b) Tracking Adria indentation beneath the Alps by detrital zircon U-Pb geochronology: Implications for the Oligocene-Miocene dynamics of the Adriatic microplate. Geology 44(2):155–158
Malusà MG, Wang J, Garzanti E, Liu ZC, Villa IM, Wittmann H (2017) Trace-element and Nd-isotope systematics in detrital apatite of the Po river catchment: Implications for provenance discrimination and the lag-time approach to detrital thermochronology. Lithos 290–291:48–59
Mange MA, Wright DT (eds) (2007) Heavy minerals in use. Elsevier, Amsterdam
Markwitz V, Kirkland CL, Mehnert A, Gessner K, Shaw J (2017) 3-D characterization of detrital zircon grains and its implications for fluvial transport, mixing, and preservation bias. Geochem Geophys Geosyst 18:4655–4673
McBride EF (1985) Diagenetic processes that affect provenance determinations in sandstones. In Zuffa GG (ed) Provenance of arenites. Dordrecht, Reidel, NATO ASI Series 148:95–113
McLennan SM, Hemming S, McDaniel DK, Hanson GN (1993) Geochemical approaches to sedimentation, provenance, and tectonics. Geol S Am S 284:21–40
Milliken KL (2007) Provenance and diagenesis of heavy minerals, Cenozoic units of the northwestern Gulf of Mexico sedimentary basin. Dev Sediment 58:247–261
Moecher DP, Samson SD (2006) Differential zircon fertility of source terranes and natural bias in the detrital zircon record: implications for sedimentary provenance analysis. Earth Planet Sci Lett 247:252–266
Morton AC (1979) Surface features of heavy mineral grains from Palaeocene sands of the central North Sea. Scot J Geol 15(4):293–300
Morton AC (2012) Value of heavy minerals in sediments and sedimentary rocks for provenance, transport history and stratigraphic correlation. Mineral Ass Canada Short Course Series 42:133–165
Morton AC, Hallsworth C (1994) Identifying provenance-specific features of detrital heavy mineral assemblages in sandstones. Sediment Geol 90(3):241–256
Morton AC, Hallsworth C (2007) Stability of detrital heavy minerals during burial diagenesis. Dev Sediment 58:215–245
Najman YMR, Pringle MS, Johnson MRW, Robertson AHF, Wijbrans JR (1997) Laser 40Ar/39Ar dating of single detrital muscovite grains from early foreland-basin sedimentary deposits in India: implications for early Himalayan evolution. Geology 25:535–538
Nasdala L, Wenzel M, Vavra G, Irmer G, Wenzel T, Kober B (2001) Metamictisation of natural zircon accumulation versus thermal annealing of radioactivity-induced damage. Contrib Mineral Petr 141:125–144
Nickel E (1973) Experimental dissolution of light and heavy minerals in comparison with weathering and intrastratal solution. Contrib Sediment 1:1–68
Pettijohn FJ, Potter PE, Siever R (1972) Sand and sandstone. Springer, New York
Pratten NA (1981) The precise measurement of the density of small samples. J Mater Sci 16:1737–1747
Reid I, Frostick LE (1985) Role of settling, entrainment and dispersive equivalence and of interstice trapping in placer formation. J Geol Soc London 142:739–746
Reiners PW, Farley KA (2001) Influence of crystal size on apatite (U–Th)/He thermochronology: an example from the Bighorn Mountains, Wyoming. Earth Planet Sci Lett 188(3):413–420
Resentini A, Malusà MG (2012) Sediment budgets by detrital apatite fission-track dating (Rivers Dora Baltea and Arc, Western Alps). Geol S Am S 487:125–140
Resentini A, Malusà MG, Garzanti E (2013) MinSORTING: An Excel® worksheet for modelling mineral grain-size distribution in sediments, with application to detrital geochronology and provenance studies. Comput Geosci 59:90–97
Rittenhouse G (1943) Transportation and deposition of heavy minerals. Geol Soc Am Bull 54:1725–1780
Rong J, Wang F (2016) Discussion about the origin of mineral textures in granite. In: Metasomatic textures in granites. Springer, Singapore
Rubey WW (1933) The size distribution of heavy minerals within a water laid sandstone. J Sediment Petr 3:3–29
Russell RD, Taylor RE (1937) Roundness and shape of Mississippi River sands. J Geol 45:225–267
Saylor JE, Knowles JN, Horton BK, Nie J, Mora A (2013) Mixing of source populations recorded in detrital zircon U-Pb age spectra of modern river sands. J Geol 121:17–33
Schuiling RD, DeMeijer RJ, Riezebos HJ, Scholten MJ (1985) Grain size distribution of different minerals in a sediment as a function of their specific density. Geol Mijnbouw 64:199–203
Silver LT, Williams IS, Woodhead JA (1981) Uranium in granites from the southwestern United States: actinide parent–daughter systems, sites and mobilization. U.S. Department of Energy Open–File Repository GJBX–45
Sircombe KN, Stern RA (2002) An investigation of artificial biasing in detrital zircon U-Pb geochronology due to magnetic separation in sample preparation. Geochim Cosmochim Ac 66:2379–2397
Slingerland R, Smith ND (1986) Occurrence and formation of water-laid placers. Annu Rev Earth Pl Sc 14:113–147
Smirnov NV (1939) On the estimation of the discrepancy between empirical curves of distribution for two independent samples. Bull Math Univ Moscow 2:3–14
Spear FS, Pyle JM (2002) Apatite, monazite, and xenotime in metamorphic rocks. Rev Mineral Geochem 48:293–335
Tagami T, Carter A, Hurford AJ (1996) Natural long termannealing of the zircon fission track system in Vienna Basin deep borehole samples: constraints upon the partial annealing zone and closure temperature. Chem Geol 130:147–157
Thiel GA (1940) The relative resistance to abrasion of mineral grains of sand size. J Sediment Res 10(3)
Thomas M, Thorp M, McAlister J (1999) Equatorial weathering, landform development and the formation of white sands in north western Kalimantan, Indonesia. CATENA 36:205–232
Tranel LM, Spotila JA, Kowalewski MJ, Waller CM (2011) Spatial variation of erosion in a small, glaciated basin in the Teton Range, Wyoming, based on detrital apatite (U-Th)/He thermochronology. Basin Res 23:571–590
Tripathy-Lang A, Hodges KV, Monteleone BD, Soest MC (2013) Laser (U-Th)/He thermochronology of detrital zircons as a tool for studying surface processes in modern catchments. J Geophys Res-Earth 118(3):1333–1341
Van Loon AJ, Mange AM (2007) “In situ” dissolution of heavy minerals through extreme weathering, and the application of the surviving assemblages and their dissolution characteristics to correlation of Dutch and German silver sands. Dev Sediment 58:189–213
Velbel MA (1999) Bond strength and the relative weathering rates of simple orthosilicates. Am J Sci 299(7–9):679–696
von Eynatten H, Dunkl I (2012) Assessing the sediment factory: the role of single grain analysis. Earth-Sci Rev 115:97–120
Walderhaug O, Porten KW (2007) Stability of detrital heavy minerals on the Norwegian continental shelf as a function of depth and temperature. J Sediment Res 77(12):992–1002
Wittmann H, Von Blanckenburg F, Maurice L, Guyot JL, Kubik PW (2011) Recycling of Amazon floodplain sediment quantified by cosmogenic 26Al and 10Be. Geology 39(5):467–470
Wittmann H, Malusà MG, Resentini A, Garzanti E, Niedermann S (2016) The cosmogenic record of mountain erosion transmitted across a foreland basin: source-to-sink analysis of in situ 10Be, 26Al and 21Ne in sediment of the Po river catchment. Earth Planet Sci Lett 452:258–271
Worden RH, Burley SD (2003) Sandstone diagenesis: the evolution of sand to stone. Sandstone Diagenesis Recent Anc 4:3–44
Young IT (1977) Proof without prejudice: use of the Kolmogorov-Smirnov test for the analysis of histograms from flow systems and other sources. J Histochem Cytochem 25:935–941
Zhang JY, Yin A, Liu WC, Wu FY, Lin D, Grove M (2012) Coupled U-Pb dating and Hf isotopic analysis of detrital zircon of modern river sand from the Yalu River (Yarlung Tsangpo) drainage system in southern Tibet: Constraints on the transport processes and evolution of Himalayan rivers. Geol Soc Am Bull 124:1449–1473
Zuffa GG (ed) (1985) Provenance of arenites. Springer, Netherlands
Acknowledgements
We are grateful to researchers and graduate students in the laboratory of fission-track analysis at University of Milano-Bicocca for their contributions in establishing the approaches described in this work. Reviews by O. Anfinson and M. L. Balestrieri, and comments by P. G. Fitzgerald were of great help to improve the clarity of the manuscript.
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Malusà, M.G., Garzanti, E. (2019). The Sedimentology of Detrital Thermochronology. In: Malusà, M., Fitzgerald, P. (eds) Fission-Track Thermochronology and its Application to Geology. Springer Textbooks in Earth Sciences, Geography and Environment. Springer, Cham. https://doi.org/10.1007/978-3-319-89421-8_7
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