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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Asia
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Far East
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Taiwan
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Taiwanese Central Range (11)
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Australasia
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New Zealand
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Haast River (1)
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Waipaoa River (1)
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North Island (1)
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Pacific Ocean
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North Pacific
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Northwest Pacific
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South China Sea
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Manila Trench (1)
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West Pacific
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Northwest Pacific
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South China Sea
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Manila Trench (1)
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South Island (1)
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Southern Alps (1)
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elements, isotopes
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carbon
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organic carbon (1)
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geochronology methods
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(U-Th)/He (1)
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Ar/Ar (1)
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fission-track dating (2)
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thermochronology (2)
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geologic age
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Cenozoic
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Quaternary
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Holocene (1)
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Pleistocene (2)
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Tertiary
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Neogene
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Pliocene (1)
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minerals
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phosphates
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apatite (2)
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silicates
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framework silicates
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feldspar group
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alkali feldspar
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adularia (1)
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orthosilicates
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nesosilicates
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zircon group
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zircon (2)
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Primary terms
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absolute age (2)
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Asia
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Far East
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Taiwan
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Taiwanese Central Range (11)
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Australasia
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New Zealand
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Haast River (1)
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Waipaoa River (1)
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carbon
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organic carbon (1)
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Cenozoic
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Quaternary
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Holocene (1)
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Pleistocene (2)
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Tertiary
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Neogene
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Pliocene (1)
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crust (2)
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deformation (3)
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earthquakes (2)
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faults (2)
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geochemistry (1)
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geochronology (1)
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geomorphology (3)
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geophysical methods (2)
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heat flow (1)
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hydrology (2)
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orogeny (2)
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Pacific Ocean
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North Pacific
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Northwest Pacific
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South China Sea
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Manila Trench (1)
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West Pacific
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Northwest Pacific
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South China Sea
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Manila Trench (1)
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plate tectonics (5)
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sedimentation (1)
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sediments (1)
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tectonics
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neotectonics (2)
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weathering (2)
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sediments
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sediments (1)
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Taiwanese Central Range
Extensional mountain building along convergent plate boundary: Insights from the active Taiwan mountain belt
Pleistocene onset of rapid, punctuated exhumation in the eastern Central Range of the Taiwan orogenic belt
Detecting Deep Tectonic Tremor in Taiwan with a Dense Array
Seasonal, long-term, and short-term deformation in the Central Range of Taiwan induced by landslides
The Shuilikeng fault in the central Taiwan mountain belt
Inversion of a hyper-extended rifted margin in the southern Central Range of Taiwan
Extreme storm events, landscape denudation, and carbon sequestration: Typhoon Mindulle, Choshui River, Taiwan
Geomorphic analysis of the Central Range fault, the second major active structure of the Longitudinal Valley suture, eastern Taiwan
The geochemistry of river water, river sediments, and suspended matter in three mountainous watersheds in New Zealand and Taiwan is used to determine chemical erosion yields in regions of rapid tectonic uplift. Suspended matter from all three rivers is depleted in soluble alkali metals and alkaline earths compared to upper continental crust material and marine clays, reflecting the bedrocks' origin as marine sediments that had undergone previous weathering cycles prior to uplift and subjection to the current chemical weathering regime. The New Zealand rivers are depleted in Mg 2+ and enriched in Ca 2+ and Na + + K + compared to global average river water, but the Taiwan river is enriched only in Mg 2+ compared to global average. The Haast compared River, draining the Southern Alps of New Zealand, is depleted in Cl + SO 4 to the global average, but has higher alkalinity and slightly higher H 4 SiO 4 . The chemical weathering yields determined here compose only a small portion (1%–5%) of the total weathering in these systems, but are still among the highest chemical yields ever reported. Our new data, in comparison to previously determined physical erosion yields in these watersheds, show that physical erosion strongly enhances chemical erosion. This work demonstrates the importance of chemical erosion as a process denuding the landscape, especially in high-standing, tectonically active mountainous landscapes.