SOUTHERN SIBERIAN PLATFORM: RECORD OF NON- SYNCHRONOUS NRM-COMPONENTS OR A NON-AXIAL GEOMAGNETIC FIELD?
The Middle Ordovician Volginsky and Kirensky fossil zones were sampled in the Krivaya Luka section (Krivolutsky suite) that outcrops along the Lena river in Siberia. The Volginsky and Kirensky zones are coeval to the Llandeilo in the global geologic time scale. The Krivaya Luka section consists of s...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.581.9374 2023-05-15T17:07:39+02:00 SOUTHERN SIBERIAN PLATFORM: RECORD OF NON- SYNCHRONOUS NRM-COMPONENTS OR A NON-AXIAL GEOMAGNETIC FIELD? Ordovician Krivolutsky Suite Krivaya Luka Section V. P. Rodionov C. E. Duermeijer D. Heslop The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.581.9374 http://www.geo.uu.nl/~forth/publications/Rodionov_2003.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.581.9374 http://www.geo.uu.nl/~forth/publications/Rodionov_2003.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.geo.uu.nl/~forth/publications/Rodionov_2003.pdf text ftciteseerx 2016-08-28T00:02:07Z The Middle Ordovician Volginsky and Kirensky fossil zones were sampled in the Krivaya Luka section (Krivolutsky suite) that outcrops along the Lena river in Siberia. The Volginsky and Kirensky zones are coeval to the Llandeilo in the global geologic time scale. The Krivaya Luka section consists of siltstones, clays, sandstones, and limestones, and displays a remarkably distinct sedimentary cyclicity, especially in its reddish middle part. Stepwise thermal demagnetization yields three NRM components. Component A, isolated in the 100−250°C interval can be either normal or reversed. The normal A-component has a direction close to recent local magnetic field. The reversed A-component directions are scattered around a direction close to that of the lower Triassic Siberian traps. Component B, has unblocking temperatures that range from 400 to 500°C and is represented mainly by normal polarity directions. The B-component, isolated from rocks of the middle part of the section is of a normal polarity with D = 176.5°, I = 30.0 ° and a North pole position at 16.2°S, 111.3°E. The other parts of the Text lena river North Pole Siberia Unknown North Pole |
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Open Polar |
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Unknown |
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ftciteseerx |
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English |
description |
The Middle Ordovician Volginsky and Kirensky fossil zones were sampled in the Krivaya Luka section (Krivolutsky suite) that outcrops along the Lena river in Siberia. The Volginsky and Kirensky zones are coeval to the Llandeilo in the global geologic time scale. The Krivaya Luka section consists of siltstones, clays, sandstones, and limestones, and displays a remarkably distinct sedimentary cyclicity, especially in its reddish middle part. Stepwise thermal demagnetization yields three NRM components. Component A, isolated in the 100−250°C interval can be either normal or reversed. The normal A-component has a direction close to recent local magnetic field. The reversed A-component directions are scattered around a direction close to that of the lower Triassic Siberian traps. Component B, has unblocking temperatures that range from 400 to 500°C and is represented mainly by normal polarity directions. The B-component, isolated from rocks of the middle part of the section is of a normal polarity with D = 176.5°, I = 30.0 ° and a North pole position at 16.2°S, 111.3°E. The other parts of the |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Ordovician Krivolutsky Suite Krivaya Luka Section V. P. Rodionov C. E. Duermeijer D. Heslop |
spellingShingle |
Ordovician Krivolutsky Suite Krivaya Luka Section V. P. Rodionov C. E. Duermeijer D. Heslop SOUTHERN SIBERIAN PLATFORM: RECORD OF NON- SYNCHRONOUS NRM-COMPONENTS OR A NON-AXIAL GEOMAGNETIC FIELD? |
author_facet |
Ordovician Krivolutsky Suite Krivaya Luka Section V. P. Rodionov C. E. Duermeijer D. Heslop |
author_sort |
Ordovician Krivolutsky Suite |
title |
SOUTHERN SIBERIAN PLATFORM: RECORD OF NON- SYNCHRONOUS NRM-COMPONENTS OR A NON-AXIAL GEOMAGNETIC FIELD? |
title_short |
SOUTHERN SIBERIAN PLATFORM: RECORD OF NON- SYNCHRONOUS NRM-COMPONENTS OR A NON-AXIAL GEOMAGNETIC FIELD? |
title_full |
SOUTHERN SIBERIAN PLATFORM: RECORD OF NON- SYNCHRONOUS NRM-COMPONENTS OR A NON-AXIAL GEOMAGNETIC FIELD? |
title_fullStr |
SOUTHERN SIBERIAN PLATFORM: RECORD OF NON- SYNCHRONOUS NRM-COMPONENTS OR A NON-AXIAL GEOMAGNETIC FIELD? |
title_full_unstemmed |
SOUTHERN SIBERIAN PLATFORM: RECORD OF NON- SYNCHRONOUS NRM-COMPONENTS OR A NON-AXIAL GEOMAGNETIC FIELD? |
title_sort |
southern siberian platform: record of non- synchronous nrm-components or a non-axial geomagnetic field? |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.581.9374 http://www.geo.uu.nl/~forth/publications/Rodionov_2003.pdf |
geographic |
North Pole |
geographic_facet |
North Pole |
genre |
lena river North Pole Siberia |
genre_facet |
lena river North Pole Siberia |
op_source |
http://www.geo.uu.nl/~forth/publications/Rodionov_2003.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.581.9374 http://www.geo.uu.nl/~forth/publications/Rodionov_2003.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766063130195001344 |