Detrital Thermochronologic Record of Burial Heating and Sediment Recycling in the Magallanes Foreland Basin, Patagonian Andes Julie C
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EAGE Basin Research (2014) 1–27, doi: 10.1111/bre.12088 Detrital thermochronologic record of burial heating and sediment recycling in the Magallanes foreland basin, Patagonian Andes Julie C. Fosdick,* Marty Grove,† Stephan A. Graham,† Jeremy K. Hourigan,‡ Oscar Lovera§ and Brian W. Romans¶ *Geological Sciences, Indiana University, Bloomington, IN, USA †Geological & Environmental Sciences, Stanford University, Stanford, CA, USA ‡Earth Sciences, University of California, Santa Cruz, CA, USA §Earth & Space Sciences, University of California, Los Angeles, CA, USA ¶Geosciences, Virginia Polytechnic Institute and State University, Blacksburg, VA, USA ABSTRACT The Patagonian Magallanes retroarc foreland basin affords an excellent case study of sediment burial recycling within a thrust belt setting. We report combined detrital zircon U–Pb geochronology and (U–Th)/He thermochronology data and thermal modelling results that confirm delivery of both rap- idly cooled, first-cycle volcanogenic sediments from the Patagonian magmatic arc and recycled sedi- ment from deeply buried and exhumed Cretaceous foredeep strata to the Cenozoic depocentre of the Patagonian Magallanes basin. We have quantified the magnitude of Eocene heating with thermal models that simultaneously forward model detrital zircon (U–Th)/He dates for best-fit thermal his- tories. Our results indicate that 54–45 Ma burial of the Maastrichtian Dorotea Formation produced 164–180 °C conditions and heating to within the zircon He partial retention zone. Such deep burial is unusual for Andean foreland basins and may have resulted from combined effects of high basal heat flow and high sediment accumulation within a rapidly subsiding foredeep that was floored by basement weakened by previous Late Jurassic rifting. In this interpretation, Cenozoic thrust-related deformation deeply eroded the Dorotea Formation from ca. 5 km burial depths and may be respon- sible for the development of a basin-wide Palaeogene unconformity. Results from the Cenozoic Rıo Turbio and Santa Cruz formations confirm that they contain both Cenozoic first-cycle zircon from the Patagonian magmatic arc and highly outgassed zircon recycled from older basin strata that experienced burial histories similar to those of the Dorotea Formation. INTRODUCTION provenance interpretations. Such factors are critical for assessing long-term sediment budgets, interactions Sedimentary basins chronicle the erosional history of between tectonics and sedimentation, nutrient flux from their sediment sources, offering invaluable information the continents into the deep sea and the distribution of about orogenic unroofing histories and inferred deforma- natural resources. tional events in diverse tectonic environments (e.g. Dick- Sediment recycling is expected in many tectonic set- inson & Suczek, 1979; Steidtmann & Schmitt, 1988). tings, such as foreland basins, where the path followed by Integration of complementary sedimentary provenance grains initially derived from erosion of a basement source methods including conglomerate and sandstone petrogra- region typically involves significant intermediate stages of phy, palaeocurrent measurements, geochemical analysis crustal evolution before the detritus is finally incorporated and detrital zircon geochronology can provide powerful into tectonically stable basin strata. Figure 1 illustrates fingerprinting of source regions (e.g. Suttner, 1974; Gra- how sediments eroded from the active thrust belt may be ham et al., 1986; Dickinson, 1988; Heller and Frost, tectonically buried beneath advancing thrusts and sedi- 1988; Degraaff-Surpless et al., 2002). In tectonically mentary overburden and later re-exhumed by thrusting complex environments such as thrust belts, however, to serve as the source terrane for younger sedimentary more information is often required to recognize sediment rocks in the basin (e.g. Schmitt & Steidtmann, 1990; Gra- recycling of lithologic units and older thrust belt ham et al., 1993). The shallow crustal histories experi- cannibalization that can lead to ambiguous sedimentary enced by eroded sediment are associated with important differences in thermal histories (Fig. 1) that go unde- Correspondence: Julie C. Fosdick, Department of Geological tected by traditional provenance methods, but are poten- Sciences, Indiana University, Bloomington, IN 47404, USA. E-mail: [email protected] tially recoverable by thermochronologic methods. © 2014 The Authors Basin Research © 2014 John Wiley & Sons Ltd, European Association of Geoscientists & Engineers and International Association of Sedimentologists 1 Julie C. Fosdick et al. Unroofing of upper crustal levels of orogenic highlands Deposition TEMPERATURE 150°C Detrital zircon cooling paths Sediment derived from Sediment-source thermal history multiple sources 150°C 150°C Burial TIME 150°C Basin burial & heating Basin exhumation Uplift and exhumation Basin historythermal of basin strata Erosion and 150°C transport to younger depocenter Fig. 1. Schematic illustration of sediment source terranes and basinfill in a typical foreland basin setting showing the thermal evolu- tion of sediment during its detrital exhumation history (upper panels) and its subsequent basin thermal history (lower panels). The Patagonian Magallanes retroarc foreland basin of thrust belt throughout the latest Cretaceous and early southern South America (Fig. 2) provides an excellent Cenozoic, it is likely that foreland basin sediment – also geologic setting to explore complex sediment and source batholith-derived – of this age experienced protracted lat- thermal histories via combined zircon U–Pb and He age est Cretaceous – early Cenozoic burial. Continued thrust dating. Many stratigraphic and provenance studies have deformation ultimately exhumed and eroded these strata focused upon the Upper Cretaceous Patagonian Magall- and reworked the detritus into younger Cenozoic depos- anes basin strata (e.g. Katz, 1963; Macellari et al., 1989; its. In some cases, Cenozoic thrust burial of Upper Creta- Biddle et al., 1986; Wilson, 1991; Fildani et al., 2003; Fil- ceous strata occurred to depths sufficient to partially dani & Hessler, 2005; Romans et al., 2010; Bernhardt degas He from zircon (Fosdick et al., 2013). et al., 2011; McAtamney et al., 2011) that have demon- Thermochronology relies upon the balance of radio- strated sustained sedimentary connectivity between the genic ingrowth and thermally activated diffusive loss of southern Patagonian batholith (Herve et al., 2007b) and daughter products of radioactive decay in minerals and the age-equivalent thrust belt and marine foredeep in the thus provides a sensitive tool for constraining tempera- Patagonian Andes. Throughout the Late Cretaceous, sed- ture–time histories. Detrital thermochronology methods iment dispersal systems provided a remarkably continu- such as 40Ar/39Ar in muscovite and K-feldspar, and fis- ous supply of batholith-sourced zircon to the basin sion track and (U–Th)/He analysis of apatite and zircon (Fig. 2). Recent work on the Palaeogene nonmarine ba- have been widely exploited to elucidate the thermal histo- sinfill also records a prominent arc source during early ries of sedimentary basins and their respective source Cenozoic Patagonian foreland basin evolution at this lati- regions (Reiners & Brandon, 2006). Combined dating of tude (Otero et al., 2012; Schwartz et al., 2012). However, two or more chronologic systems with differing tempera- the detailed path taken by this batholith-derived detritus ture sensitivity in the same phase can significantly remains unclear. Because of the tectonic activity of the increase the ability to interpret detrital thermochronology © 2014 The Authors 2 Basin Research © 2014 John Wiley & Sons Ltd, European Association of Geoscientists &EngineersandInternationalAssociationofSedimentologists Detrital thermochronology of the Magallanes basin Uplifted Cretaceous Magallanes Basin detrital zircon age distribution (n = 550) 48°S Pacific Ocean NPK3 K2 K1 J h c n e r T Pz-Mz mb e l i h 0 25 50 75 100 125 150 175 200 C U-Pb age (Ma) ICE IAN ON Relative probability distribution G TH RVB us TA LI o PA HO e 02004006008001000120014001600 AT c B ta l e il U-Pb age (Ma) r -f C in s d a e b ft li s p e n U a ll a Atlantic Ocean g a M Figure 4 51°S PALEOGEOGRAPHY Drainage divide IC O S A Z E A’ Cretaceous sediment O N EN A dispersal direction C LL GA Oligocene-Miocene position of A-A’ A IN M S sediment dispersal schematic crustal A section Fig. 14 B LITHOTECTONIC UNITS RVB Cenozoic foreland basin-fill Patagonian thrust-belt Patagonian batholith Late Jurassic bimodal volcanics Paleozoic & Mesozoic metamorphic basement (Pz-Mz mb) BATHOLITH INTRUSIVE AGES Neogene (25-15 Ma) Paleogene (67-40 Ma) Late Cretaceous (126-70 Ma) Mid Cretaceous (136-127 Ma) 0 100 km Early Cretaceous (144-137 Ma) 70°W Jurassic plutons (157-145 Ma) Fig. 2. Tectonostratigraphic map of the southern Patagonian Andes showing the location of the study area (Fig. 4). Triangles show pluton ages of the Patagonian batholith, a major sediment source to the foreland basin (intrusive intervals defined by Herve et al., 2007b). Grey arrows indicate general sediment dispersal patterns for the Late Cretaceous basin (solid) and Oligo- cene–Miocene basin (dashed). Inset: compiled detrital U–Pb age distributions from the Patagonian Cretaceous Magallanes basin (compiled from Fildani et al., 2003; Romans et al., 2010; Bernhardt et al., 2011) in comparison to the batholith intrusive ages (shown by coloured panels). results. Consequently,