Log in

Relevant bibliographies by topics / Continental denudation

Contents

Journal articles

Academic literature on the topic 'Continental denudation'

Author: Grafiati

Published: 4 June 2021

Last updated: 8 February 2022

Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles

Select a source type:

Consult the lists of relevant articles, books, theses, conference reports, and other scholarly sources on the topic 'Continental denudation.'

Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.

You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.

Journal articles on the topic "Continental denudation"

1

HOWELL, D. G., and R. W. MURRAY. "A Budget for Continental Growth and Denudation." Science 233, no. 4762 (1986): 446–49. http://dx.doi.org/10.1126/science.233.4762.446.

Full text

APA, Harvard, Vancouver, ISO, and other styles

2

Willenbring, J. K., A. T. Codilean, K. L. Ferrier, B. McElroy, and J. W. Kirchner. "Short Communication: Earth is (mostly) flat, but mountains dominate global denudation: apportionment of the continental mass flux over millennial time scales, revisited." Earth Surface Dynamics Discussions 2, no. 1 (2014): 1–17. http://dx.doi.org/10.5194/esurfd-2-1-2014.

Full text

Abstract:

Abstract. Carbon dioxide consumption by silicate mineral weathering and the subsequent precipitation of carbonate sediments sequesters CO2 over geologic timescales. The rate of this carbon sequestration is coupled to rates of continental erosion, which exposes fresh minerals to weathering. Steep mountain landscapes represent a small fraction of continental surfaces but contribute disproportionately to global erosion rates. However, the relative contributions of Earth's much vaster, but more slowly eroding, plains and hills remain the subject of debate. Recently, Willenbring et al. (2013) analy

APA, Harvard, Vancouver, ISO, and other styles

3

Jelinek, Andrea Ritter. "Evolução Paleotopográfica da Margem Continental Brasileira durante o Fanerozoico: Evidências a partir da Termocronologia por Traços de Fissão em Apatitas (Paleotopographic Evolution of the Brazilian Continental Margin during the Phanerozoic: Evidence from Apatite Fission Track Thermochronology)." Revista Brasileira de Geografia Física 12, no. 4 (2019): 1670. http://dx.doi.org/10.26848/rbgf.v12.4.p1670-1686.

Full text

Abstract:

Este trabalho explora banco de dados traços de fissão em apatitas com o objetivo de desenvolver uma visão sinóptica de padrões de denudação através do espaço-tempo na margem continental brasileira. A resposta geomorfológica aos processos de rifteamento e ruptura continental variou ao longo da margem continental brasileira. No processo de construção do relevo desta margem foram registrados três episódios de resfriamento acelerado, que são vinculados a processos denudacionais: Cretáceo Inferior, Cretáceo Superior e Paleógeno-Neógeno. As margens continentais sudeste e leste apresentam uma morfolo

APA, Harvard, Vancouver, ISO, and other styles

4

Lisker, Frank, Christopher J. L. Wilson, and Helen J. Gibson. "Thermal history of the Vestfold Hills (East Antarctica) between Lambert rifting and Gondwana break-up, evidence from apatite fission track data." Antarctic Science 19, no. 1 (2007): 97–106. http://dx.doi.org/10.1017/s0954102007000144.

Full text

Abstract:

Analysis of five basement samples from the Vestfold Hills (East Antarctica) reveals pooled apatite fission track (FT) ages ranging from 188 to 264 Ma and mean lengths of 13.7 to 14.9 μm. Quantitative thermal histories derived from these data give consistent results indicating onset of cooling/denudation began sometime prior to 240 Ma, with final cooling below 105°–125°C occurring between 240 and 220 Ma (Triassic). A Cretaceous denudation phase can be inferred from the sedimentary record of the Prydz Bay offshore the Vestfold Hills. The two denudational episodes are likely associated with Palae

APA, Harvard, Vancouver, ISO, and other styles

5

Codilean, A. T., R. H. Fülöp, H. Munack, et al. "Controls on denudation along the East Australian continental margin." Earth-Science Reviews 214 (March 2021): 103543. http://dx.doi.org/10.1016/j.earscirev.2021.103543.

Full text

APA, Harvard, Vancouver, ISO, and other styles

6

Bishop, Paul. "Southeast Australian late Mesozoic and Cenozoic denudation rates: A test for late Tertiary increases in continental denudation." Geology 13, no. 7 (1985): 479. http://dx.doi.org/10.1130/0091-7613(1985)13<479:salmac>2.0.co;2.

Full text

APA, Harvard, Vancouver, ISO, and other styles

7

Kerr, Andrew, and Alan Gilchrist. "Glaciation, erosion and the evolution of the Transantarctic Mountains, Antarctica." Annals of Glaciology 23 (1996): 303–8. http://dx.doi.org/10.1017/s0260305500013574.

Full text

Abstract:

Modelling studies of the tectonic evolution of the Transantarctic Mountains in Antarctica have drawn differing conclusions as to the primary mechanisms involved. None has considered the role of the East Antarctic ice sheet in detail. We use a denudation—flexural model to examine the isostatic response of the continental margin to glacial erosion to determine whether glacial processes have played a role in forcing mountain uplift. The conclusion is that, although there are insufficient data formally to delimit the role of glacial erosion, available geophysical and geomorphological data are not

APA, Harvard, Vancouver, ISO, and other styles

8

Kerr, Andrew, and Alan Gilchrist. "Glaciation, erosion and the evolution of the Transantarctic Mountains, Antarctica." Annals of Glaciology 23 (1996): 303–8. http://dx.doi.org/10.3189/s0260305500013574.

Full text

Abstract:

Modelling studies of the tectonic evolution of the Transantarctic Mountains in Antarctica have drawn differing conclusions as to the primary mechanisms involved. None has considered the role of the East Antarctic ice sheet in detail. We use a denudation—flexural model to examine the isostatic response of the continental margin to glacial erosion to determine whether glacial processes have played a role in forcing mountain uplift.The conclusion is that, although there are insufficient data formally to delimit the role of glacial erosion, available geophysical and geomorphological data are not i

APA, Harvard, Vancouver, ISO, and other styles

9

Kravchuk, Yaroslav, and Vasyl Chalyk. "PRECARPATHIAN AND TRANSCARPATHIAN LANDFORM EVOLUTION IN THE PLIOCENE-PLEOSTOCENE AND AT EARLY STAGES." PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS, no. 09 (01) (September 25, 2019): 154–65. http://dx.doi.org/10.30970/gpc.2019.1.2808.

Full text

Abstract:

The Sarmatian-Pannonian and Pontian-Pliocene stages are most important in the landform evolution of the Inner Precarpathians and Solotvyn basin. Due to the intense elevations in the upper Miocene, the Precarpathian Sea was pushed to the east and northeast. On the land freed from the sea, a hydrographic network was created, and rivers moved along the retreating sea in Northeast and Southeast directions. Original river valleys were of diagonal and inline outflow directions unlike modern transverse valleys. The Pontian-Pliocene is associated with the final phase of Carpathian and Precarpathian te

APA, Harvard, Vancouver, ISO, and other styles

10

Dokka, RoyK, and MichaelJ Mahaffie. "Tectonic denudation: The forgotten mechanism for rapid cooling of continental interiors." Nuclear Tracks and Radiation Measurements (1982) 10, no. 3 (1985): 407. http://dx.doi.org/10.1016/0735-245x(85)90136-x.

Full text

APA, Harvard, Vancouver, ISO, and other styles

More sources

We offer discounts on all premium plans for authors whose works are included in thematic literature selections. Contact us to get a unique promo code!