Patterns of denudation through time in the San Bernardino Mountains, California: Implications for early-stage orogenesis

被引:25
作者
Binnie, Steven A. [1 ]
Phillips, William M. [1 ]
Summerfield, Michael A. [1 ]
Fifield, L. Keith [2 ]
Spotila, James A. [3 ]
机构
[1] Univ Edinburgh, Inst Geog, Edinburgh EH8 9XP, Midlothian, Scotland
[2] Australian Natl Univ, Dept Nucl Phys, Res Sch Phys Sci & Engn, Canberra, ACT 0200, Australia
[3] Virginia Polytech Inst & State Univ, Dept Geosci, Blacksburg, VA 24061 USA
关键词
denudation rates; topographic evolution; cosmogenic nuclides; orogenesis; San Bernardino Mountains;
D O I
10.1016/j.epsl.2008.09.008
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Basin-averaged cosmogenic Be-10 concentrations, apatite (U-Th)/He thermochronometry and incision into a dated palaeosurface constrain spatial and temporal variations in the rates of denudation experienced during the early-stages of orogenesis in the San Bernardino Mountains, California. Cosmogenic Be-10 analysis measures denudation over intermediate (similar to 10(2)-10(4) years) time scales and records rates which decrease from a maximum of 2700 +/- 500 mm ka(-1) in the south to a minimum of 52 +/- 5 mm ka(-1) in northern catchments. Corresponding rates from (U-Th)/He and incision into a dated palaeosurface measure long-term (similar to 10(6) years) denudation rates which decrease from between 1200 +/- 400 mm ka(-1) in the south to a minimum of 30 20 mm ka(-1) in the north. The temporal consistency observed in the broad-scale patterns of denudation rates probably results from the persistent imprint of the initial crustal architecture and drainage network. These have maintained an influence on slope distributions, and are thus fundamental factors controlling the gross patterns of denudation throughout the early stages of orogenesis. Where variations between the denudation rates measured over different time scales are apparent the intermediate-term rates are found to be consistently greater than the long-term, with the increase being more pronounced around the fault bounded peripheries of crustal blocks relative to quiescent block interiors. This provides empirical support for a model of mountain building whereby topographic development is dictated by the headward retreat of drainage systems that propagate away from zones of displacement. Our findings indicate that recent localised increases in denudation rates in young fault block orogens may be explained by a progressive denudational response to prior tectonic uplift, rather than a consequence of climatic change. (C) 2008 Elsevier B.V. All rights reserved.
引用
收藏
页码:62 / 72
页数:11
相关论文
共 67 条
  • [1] LOCAL RELIEF AND THE HEIGHT LIMITS OF MOUNTAIN RANGES
    AHNERT, F
    [J]. AMERICAN JOURNAL OF SCIENCE, 1984, 284 (09) : 1035 - 1055
  • [2] Atwater T., 1970, GEOL SOC AM BULL, V181, P3513, DOI [10.1130/0016-7606(1970)81[3513:IOPTFT]2.0.CO
  • [3] 2, DOI 10.1130/0016-7606(1970)81[3513:IOPTFT]2.0.CO
  • [4] 2, 10.1130/0016-7606, DOI 10.1130/0016-7606]
  • [5] Latitudinal variation of denudation in the evolution of the Bolivian Andes
    Barnes, Jason B.
    Pelletier, Jon D.
    [J]. AMERICAN JOURNAL OF SCIENCE, 2006, 306 (01) : 1 - 31
  • [6] Tectonic uplift, threshold hillslopes, and denudation rates in a developing mountain range
    Binnie, Steven A.
    Phillips, William M.
    Summerfield, Michael A.
    Fifield, L. Keith
    [J]. GEOLOGY, 2007, 35 (08) : 743 - 746
  • [7] Sediment mixing rapidly and basin-wide cosmogenic nuclide analysis in eroding mountainous environments
    Binnie, Steven A.
    Phillips, William M.
    Summerfield, Michael A.
    Fifield, L. Keith
    [J]. QUATERNARY GEOCHRONOLOGY, 2006, 1 (01) : 4 - 14
  • [8] BIRD P, 1984, GEOL SOC AM BULL, V95, P946, DOI 10.1130/0016-7606(1984)95<946:KOPCAM>2.0.CO
  • [9] 2
  • [10] BLYTHE AE, 2002, CONTRIBUTIONS CRUSTA, V365, P231