Weichselian and Holocene climate history reflected in temperatures in the upper crust of the Netherlands

M. ter Voorde; R.T. van Balen; E. Luijendijk; H. Kooi

doi:10.1017/njg.2014.9

Weichselian and Holocene climate history reflected in temperatures in the upper crust of the Netherlands

M. ter Voorde, R.T. van Balen, E. Luijendijk, H. Kooi

Research output: Contribution to Journal › Article › Academic › peer-review

Abstract

In the Netherlands the present-day thermal gradient in the shallow subsurface (i.e. the upper few 100 m), is around 20°C km

Original language	English
Pages (from-to)	107-117
Journal	Netherlands Journal of Geosciences = Geologie en Mijnbouw
Volume	93
Issue number	3
DOIs	https://doi.org/10.1017/njg.2014.9
Publication status	Published - 2014

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10.1017/njg.2014.9

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@article{7e6c7e9532aa4ebfb08bb547a1a8c137,

title = "Weichselian and Holocene climate history reflected in temperatures in the upper crust of the Netherlands",

abstract = "In the Netherlands the present-day thermal gradient in the shallow subsurface (i.e. the upper few 100 m), is around 20°C km",

author = "{ter Voorde}, M. and {van Balen}, R.T. and E. Luijendijk and H. Kooi",

year = "2014",

doi = "10.1017/njg.2014.9",

language = "English",

volume = "93",

pages = "107--117",

journal = "Geologie en Mijnbouw",

issn = "0016-7746",

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AU - ter Voorde, M.

AU - van Balen, R.T.

AU - Luijendijk, E.

AU - Kooi, H.

PY - 2014

Y1 - 2014

N2 - In the Netherlands the present-day thermal gradient in the shallow subsurface (i.e. the upper few 100 m), is around 20°C km

AB - In the Netherlands the present-day thermal gradient in the shallow subsurface (i.e. the upper few 100 m), is around 20°C km

U2 - 10.1017/njg.2014.9

DO - 10.1017/njg.2014.9

M3 - Article

VL - 93

SP - 107

EP - 117

JO - Geologie en Mijnbouw

JF - Geologie en Mijnbouw

SN - 0016-7746

IS - 3

ER -

Weichselian and Holocene climate history reflected in temperatures in the upper crust of the Netherlands

Abstract

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