Linking orography , climate , and exhumation across the central Andes

نویسندگان

  • Jason B. Barnes
  • Todd A. Ehlers
  • Nadja Insel
  • Nadine McQuarrie
  • Christopher J. Poulsen
چکیده

Quantifying interactions between uplift, climate, deformation, and exhumation remains diffi cult, in many cases due to a paucity of data relevant to all processes. We synthesize new and existing data to understand the orogen-scale orographic changes across the central Andes, Bolivia. We use a regional climate model and geo-thermochronologic data to identify the correlations between changes in precipitation due to surface uplift and spatiotemporal patterns of deformation and erosional exhumation. Mean orographic rainfall patterns do not reach near present-day gradients and values until the topography grows to >75% modern elevations. New fi ssion-track data near the orocline apex indicate that rapid exhumation moved eastward, beginning in the Eastern Cordillera ca. 50–15 Ma, the Interandean zone ca. 18–6 Ma, and in the Subandes ca. 7–3 Ma. Throughout Bolivia, exhumation is consistent with deformation until ca. 15–11 Ma, after which the pattern corresponds better with the increased rainfall toward modern values. These linked observations suggest that ca. 15–11 Ma, regional elevations reached threshold values (>75% modern) necessary to generate near present-day, enhanced rainfall gradients. These gradients have resulted in variable exhumation implied by the structural level of rocks exposed across the thrust belt and confi rmed by fi ssion tracks in apatite. The main insight is that the climate-induced Middle Miocene–recent exhumation varies over scales of a few hundred kilometers across Bolivia and implies that high mean rainfall (>~3 m/yr) and long time scales (~10 m.y.) may be necessary for climate to induce orographically driven exhumation patterns recorded by fi ssion tracks. GEOLOGY, December 2012; v. 40; no. 12; p. 1–4; Data Repository item 2012328 | doi:10.1130/G33229.1 | Published online XX Month 2012 © 2012 eological Soci ty of America. For ermission to copy, contact Copyright Permissions, GSA, or [email protected]. SA FL IA EC AL SA FL IA EC AL Bolivia Peru Lake Titicaca Lake Titicaca

برای دانلود رایگان متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

ثبت نام

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

منابع مشابه

Strong tectonic and weak climatic control on exhumation rates in the 1

16 17 We have studied the relationships between present day relief, precipitation, stream power, 18 seismic energy, seismic strain rate and long-term exhumation rates for the Venezuelan Andes. 19 Average long-term exhumation rates were determined for seven large catchments in the 20 Venezuelan Andes from fission-track analysis of detrital apatite. A quantitative comparison 21 between eight new ...

متن کامل

Geometric, kinematic, and erosional history of the central Andean Plateau, Bolivia (15–17 S)

[1] Latitudinal changes in topography, climate, and thrust belt geometry in the central Andes have led to conflicting hypotheses that climate or tectonics exert a first-order control on orogen evolution. The relative roles of climate and tectonics in the evolution of the Andean orogen are difficult to quantify because of a lack of detailed observations for both the long-term deformation and ero...

متن کامل

Cenozoic paleogeography of the eastern Andean foreland and adjacent hinterland in the Colombian Northern Andes: AAPG

s (underlined = graduate student; * = postdoctoral scholar) [128] Anderson, R.B., Long, S.P., Horton, B.K., Calle, A., and Stockli, D.F., 2014, New apatite and zircon (UTh)/He constraints on the timing of thrust-related exhumation in the southern Bolivian (21 ̊S) Andes: AGU Fall Meeting. [127] Barber, D., Stockli, D.F., Koshnaw, R.I., Horton, B.K., and Kendall, J.J., 2014, Detrital zircon U-Pb a...

متن کامل

Effects of the Andes on Eastern Pacific Climate: A Regional Atmospheric Model Study*

A regional atmospheric model is used to study the effects of the narrow and steep Andes on the eastern Pacific climate. In the Southern Hemisphere cold season (i.e., August–October 1999), the model reproduces key climatic features, including the intertropical convergence zone (ITCZ) north of the equator and an extensive low-level cloud deck capped by a temperature inversion to the south. Blocki...

متن کامل

ذخیره در منابع من


  با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید

عنوان ژورنال:

دوره   شماره 

صفحات  -

تاریخ انتشار 2012