Silicate weathering as a feedback and forcing in Earth's climate and carbon cycle
Current understanding of the long-term carbon cycle posits that Earth's climate is stabilized
by a negative feedback involving CO 2 consumption by chemical weathering of silicate …
by a negative feedback involving CO 2 consumption by chemical weathering of silicate …
A Cenozoic Record of Deep Oceanic Zn Isotopic Composition in Ferromanganese Crusts
M Zhao, N Planavsky, X Wang, Y Zhang… - American Journal of …, 2023 - ajsonline.org
Water plays a critical role in erosion and sediment transport and this relationship is most
evident in the hyperarid Atacama Desert of Northern Chile, a region characterized by …
evident in the hyperarid Atacama Desert of Northern Chile, a region characterized by …
Cenozoic carbon cycle imbalances and a variable weathering feedback
The long-term stability of Earth's climate and the recovery of the ocean–atmosphere system
after carbon cycle perturbations are often attributed to a stabilizing negative feedback …
after carbon cycle perturbations are often attributed to a stabilizing negative feedback …
Monsoon controls on sediment generation and transport: Mass budget and provenance constraints from the Indus River catchment, delta and submarine fan over …
How well do deep-sea sedimentary archives track erosion in upland sources, driven by
climatic change or tectonic forcing? Located on the western edge of South Asian monsoon …
climatic change or tectonic forcing? Located on the western edge of South Asian monsoon …
Emergence of the Southeast Asian islands as a driver for Neogene cooling
Steep topography, a tropical climate, and mafic lithologies contribute to efficient chemical
weathering and carbon sequestration in the Southeast Asian islands. Ongoing arc–continent …
weathering and carbon sequestration in the Southeast Asian islands. Ongoing arc–continent …
Sulfate sulfur isotopes and major ion chemistry reveal that pyrite oxidation counteracts CO2 drawdown from silicate weathering in the Langtang-Trisuli-Narayani River …
Drawdown of atmospheric carbon dioxide (CO 2) due to silicate weathering in the Himalaya
has previously been implicated in Cenozoic cooling. However, over timescales shorter than …
has previously been implicated in Cenozoic cooling. However, over timescales shorter than …
A review of Himalayan stratigraphy, magmatism, and structure
AJ Martin - Gondwana Research, 2017 - Elsevier
Abstract The Himalayan Orogen consists of two rock packages that parallel the topographic
trend of the mountain belt between the eastern and western syntaxes. To avoid confusion …
trend of the mountain belt between the eastern and western syntaxes. To avoid confusion …
Cambrian–ordovician orogenesis in Himalayan equatorial Gondwana
PM Myrow, NC Hughes, NR McKenzie… - …, 2016 - pubs.geoscienceworld.org
An early Paleozoic tectonic event, the Kurgiakh orogeny, has long been known from the
western Tethyan Himalaya, and it is conspicuously recorded by an angular unconformity …
western Tethyan Himalaya, and it is conspicuously recorded by an angular unconformity …
Constraints on the collision and the pre-collision tectonic configuration between India and Asia from detrital geochronology, thermochronology, and geochemistry …
Abstract Knowledge of the timing of India–Asia collision is a fundamental prerequisite for
understanding the evolution of the Himalayan–Tibetan orogen and its role in global climate …
understanding the evolution of the Himalayan–Tibetan orogen and its role in global climate …
Zircon U‐Pb ages and Hf isotopes of the Askot klippe, Kumaun, northwest India: Implications for Paleoproterozoic tectonics, basin evolution and associated …
Throughout the Himalayan thrust belt, klippen of questionable tectonostratigraphic affinity
occur atop Lesser Himalayan rocks. Integrated U‐Pb ages, Hf isotopic, and whole rock trace …
occur atop Lesser Himalayan rocks. Integrated U‐Pb ages, Hf isotopic, and whole rock trace …