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词汇 varve
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Examples of varve


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Quaternary varves are used in stratigraphy and palaeoclimatology to reconstruct climate changes during the last few hundred thousand years.
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Of the many rhythmites found in the geological record, varves are among the most important and illuminating to studies of past climate change.
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Of the many rhythmites found in the geological record, varves are one of the most important and illuminating to studies of past climate change.
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Similar seasonal patterns also occur in ice cores and in varves (layers of sediment deposition in a lake, river, or sea bed).
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Each pair of layers is called a varve and represents one year.
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Varves have recently experienced a renaissance as methods and techniques of study have improved, and varves are now regularly used to calibrate radiocarbon timescales.
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In addition to seasonal variation of sedimentary processes and deposition, varve formation requires the absence of bioturbation.
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The mean thickness of a varve here is 0.18 mm, with a minimum thickness of 0.014 mm and maximum of 9.8 mm.
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Each band is similar to a varve, to the extent that the banding is assumed to result from cyclic variations in available oxygen.
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Such varves in meromictic lakes preserve an historical record something like tree rings do.
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Laminae that represent seasonal changes (similar to tree rings) are called varves.
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Varve (or "varved clay") is clay with visible annual layers, which form from seasonal differences in erosion and organic content.
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As the varves get closer to the shoreline the clay layer will stay relatively the same thickness, but there will be an increase in thickness of the silt layer.
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However, international interest in varves diminished.
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This naturally occurring anoxic basin allows for sediments to be deposited without bioturbation, forming varves of alternating light and dark color, which correspond to the dry or rainy season.
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The varves thus record the change in the lakes' environment around 1800, when the primeval forests in the region were replaced by open fields and farmland.
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At the deep permanent lake stage in a typical cycle there is normally a laminite, consisting of fine-scale alternations of clastic, carbonate and organic laminae, thought to represent annual varves.
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There is a distinct change in the color of the varves that occurred around 1800; the lower, older varves are dark brown, and the higher, younger varves are grey.
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The clays show a rhythmical, varve-like layering.
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