The Proterozoic (1.85 Ga) Älvestorp Conglomerate, Bergslagen, Central Sweden

G. Kuipers, F.F. Beunk

Research output: Contribution to JournalArticleAcademicpeer-review

Abstract

The Älvestorp conglomerates, deposited in an alluvial fan setting, form part of the Svecofennian orogenic belt in west Bergslagen, south central Sweden and are estimated to be as old as c. 1.85 Ga. Reaching a thickness of one kilometre, their architecture and form suggest an alluvial origin. Along sections, massive conglomerates often grade into pebbly mudstones and greenschist facies slates, while pure slates with dolomite concretions and olistolites occur in dark slatey mudstones on the eastern shore of lake Brunnsjön. Inner fan trenches are filled with massive, clast-supported conglomerates that contain more than 80 percent epiclastic tuffaceous material. The Älvestorp conglomerate is therefore classified as the product of a Proterozoic stream-flow channel and debris flow, or alluvial fan. The Grythyttan Basin to the north originated by extension after the first of two orogenic stages of Bergslagen.
Original languageEnglish
Article number6
Pages (from-to)222-226
JournalGeology Today
Issue number30
DOIs
Publication statusPublished - 2014

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conglomerate
Proterozoic
alluvial fan
mudstone
Svecofennian
concretion
channel flow
greenschist facies
orogenic belt
debris flow
clast
trench
streamflow
dolomite
lake
basin

Cite this

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title = "The Proterozoic (1.85 Ga) {\"A}lvestorp Conglomerate, Bergslagen, Central Sweden",
abstract = "The {\"A}lvestorp conglomerates, deposited in an alluvial fan setting, form part of the Svecofennian orogenic belt in west Bergslagen, south central Sweden and are estimated to be as old as c. 1.85 Ga. Reaching a thickness of one kilometre, their architecture and form suggest an alluvial origin. Along sections, massive conglomerates often grade into pebbly mudstones and greenschist facies slates, while pure slates with dolomite concretions and olistolites occur in dark slatey mudstones on the eastern shore of lake Brunnsj{\"o}n. Inner fan trenches are filled with massive, clast-supported conglomerates that contain more than 80 percent epiclastic tuffaceous material. The {\"A}lvestorp conglomerate is therefore classified as the product of a Proterozoic stream-flow channel and debris flow, or alluvial fan. The Grythyttan Basin to the north originated by extension after the first of two orogenic stages of Bergslagen.",
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The Proterozoic (1.85 Ga) Älvestorp Conglomerate, Bergslagen, Central Sweden. / Kuipers, G.; Beunk, F.F.

In: Geology Today, No. 30, 6, 2014, p. 222-226.

Research output: Contribution to JournalArticleAcademicpeer-review

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AU - Kuipers, G.

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AB - The Älvestorp conglomerates, deposited in an alluvial fan setting, form part of the Svecofennian orogenic belt in west Bergslagen, south central Sweden and are estimated to be as old as c. 1.85 Ga. Reaching a thickness of one kilometre, their architecture and form suggest an alluvial origin. Along sections, massive conglomerates often grade into pebbly mudstones and greenschist facies slates, while pure slates with dolomite concretions and olistolites occur in dark slatey mudstones on the eastern shore of lake Brunnsjön. Inner fan trenches are filled with massive, clast-supported conglomerates that contain more than 80 percent epiclastic tuffaceous material. The Älvestorp conglomerate is therefore classified as the product of a Proterozoic stream-flow channel and debris flow, or alluvial fan. The Grythyttan Basin to the north originated by extension after the first of two orogenic stages of Bergslagen.

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