Cambio ambiental del Cuaternario Tardio en depositos lacustres en la cuenca de Zacapu, Michoacan. Reconstruccion preliminar

S. E. Metcalfe; S. P. Harrison

Cambio ambiental del Cuaternario Tardio en depositos lacustres en la cuenca de Zacapu, Michoacan. Reconstruccion preliminar

Translated title of the contribution: Atmospheric change of the Late Quaternary in lacustrine deposits in Zacapu Basin, Michoacan. Preliminary reconstruction

S. E. Metcalfe, S. P. Harrison

Research output: Contribution to journal › Article › peer-review

5 Citations (Scopus)

Abstract

Lacustrine diatomites are intercalated with beach sands, organic marsh soils and colluvial deposits. Such a sequence reflects fluctuations in lake level and changes in the relative importance of lacustrine and terrestrial processes within the basin. The examination of these sections in terms of sediment source environment provides one means of evaluating the relative importance of specific factors, such as climatic change or the impact of man, in causing the fluctuations recorded by the deposits.-from English summary

Translated title of the contribution	Atmospheric change of the Late Quaternary in lacustrine deposits in Zacapu Basin, Michoacan. Preliminary reconstruction
Original language	Spanish
Pages (from-to)	127-151
Number of pages	25
Journal	Boletin - Instituto de Geografia, Universidad Nacional Autonoma de Mexico
Volume	14
Publication status	Published - 1984

Cite this

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title = "Cambio ambiental del Cuaternario Tardio en depositos lacustres en la cuenca de Zacapu, Michoacan. Reconstruccion preliminar",

abstract = "Lacustrine diatomites are intercalated with beach sands, organic marsh soils and colluvial deposits. Such a sequence reflects fluctuations in lake level and changes in the relative importance of lacustrine and terrestrial processes within the basin. The examination of these sections in terms of sediment source environment provides one means of evaluating the relative importance of specific factors, such as climatic change or the impact of man, in causing the fluctuations recorded by the deposits.-from English summary",

author = "Metcalfe, {S. E.} and Harrison, {S. P.}",

year = "1984",

language = "Spanish",

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pages = "127--151",

journal = "Boletin - Instituto de Geografia, Universidad Nacional Autonoma de Mexico",

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T1 - Cambio ambiental del Cuaternario Tardio en depositos lacustres en la cuenca de Zacapu, Michoacan. Reconstruccion preliminar

AU - Metcalfe, S. E.

AU - Harrison, S. P.

PY - 1984

Y1 - 1984

N2 - Lacustrine diatomites are intercalated with beach sands, organic marsh soils and colluvial deposits. Such a sequence reflects fluctuations in lake level and changes in the relative importance of lacustrine and terrestrial processes within the basin. The examination of these sections in terms of sediment source environment provides one means of evaluating the relative importance of specific factors, such as climatic change or the impact of man, in causing the fluctuations recorded by the deposits.-from English summary

AB - Lacustrine diatomites are intercalated with beach sands, organic marsh soils and colluvial deposits. Such a sequence reflects fluctuations in lake level and changes in the relative importance of lacustrine and terrestrial processes within the basin. The examination of these sections in terms of sediment source environment provides one means of evaluating the relative importance of specific factors, such as climatic change or the impact of man, in causing the fluctuations recorded by the deposits.-from English summary

UR - http://www.scopus.com/inward/record.url?scp=0021533910&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:0021533910

VL - 14

SP - 127

EP - 151

JO - Boletin - Instituto de Geografia, Universidad Nacional Autonoma de Mexico

JF - Boletin - Instituto de Geografia, Universidad Nacional Autonoma de Mexico

ER -

Cambio ambiental del Cuaternario Tardio en depositos lacustres en la cuenca de Zacapu, Michoacan. Reconstruccion preliminar

Abstract

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