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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 OpenAlexaff
K.X. Whipple, N. M. Gasparini

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

fetched live from OpenAlex

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 (~18°S) 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.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.001
metaresearch head score (Gemma)0.001
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.129
Threshold uncertainty score0.257

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0010.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.002
Science and technology studies0.0010.001
Scholarly communication0.0020.000
Open science0.0000.001
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

Classification

machine, unvalidated

Machine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations65
Published2014
Admission routes1
Has abstractyes

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