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Record W2126210028 · doi:10.1130/l325.1

Tectonic control of topography, rainfall patterns, and erosion during rapid post–12 Ma uplift of the Bolivian Andes

2014· article· en· W2126210028 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.

Bibliographic record

VenueLithosphere · 2014
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsCanadian Institute for Advanced Research
Fundersnot available
KeywordsGeologyForeland basinTectonicsFluvialErosionLandformGeomorphologyPaleontologyChannel (broadcasting)Physical geographyStructural basinGeography

Abstract

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We integrate analysis of present-day topography with a synthesis of current knowledge of the geology, deformation history, exhumation history, and the pattern of erosion rates to address the controversies surrounding the surface uplift history of the Bolivian Andes and the relative roles of climate and tectonics in the evolution of this mountainous landscape. Using metrics of channel steepness (k sn , a measure of channel slope normalized by drainage area), local relief (over a 2.5 km radius), and hillslope gradient we identify and map a suite of previously unrecognized perched, low-relief upland landscape patches in northern Bolivia that define a long-wavelength (~300 km) topographic ramp with an ~3.5 km elevation drop from SE to NW. We interpret these low-relief patches as the remnants of a formerly continuous lowrelief landscape formed on grade with the foreland that has been uplifted and warped since formation. The 11-7 Ma Cangalli Formation onlaps the northern end of this ramp and suggests a shared history and common baselevel with the well-known ca. 12-9 Ma San Juan del Oro erosion surface in southern Bolivia. Patterns of rock and surface uplift rate implied by this interpretation are consistent with those inferred independently from analysis of channel steepness (k sn ), the distribution of fluvial hanging valleys, reconstruction of channel profiles, and the distribution of published low temperature thermochronometric ages. These data reinforce earlier interpretations for 2-3 km surface uplift in the Bolivian Andes in the last 12 Ma. The marked contrast in topography across the Santa Cruz bend (~18S) appears largely controlled by differences in tectonics conditioned by inherited geologic contrasts and we show that post-12 Ma erosion and exhumation in northern Bolivia are controlled primarily by tectonics, not climate. However, the pattern and style of uplift in many locations suggests warping over deep structures in absence of significant shortening, consistent with the observation that exhumation patterns cease to be coupled to patterns of contractile deformation post-11-15 Ma. Tectonically controlled topography strongly focuses rainfall and may enhance erosional efficiency and thus erosion rates in zones of high rainfall, but no data from this study area demands this. Moreover, we find no evidence for a tectonic response to the modern rainfall pattern. We speculate that differences in the pattern of deformation and uplift across the Santa Cruz bend appear to be accommodated by a crustal-scale relay ramp.

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Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.004
Threshold uncertainty score0.999

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.005
GPT teacher head0.188
Teacher spread0.183 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it