A magnetostratigraphic profile of the uppermost Tatarian (Upper Permian) of a section of continental sediments from Eastern Platform is presented. Around 300 samples across an Upper Permian sequence o f red beds Monastirskoje on the Volga River Valley (South-West of Tatarian, Russia) have been collected. The characteristic primary component defined nearly for all the examined samples has a normal as well as reversed polarity, therefore a clear polarity zonation Is defined. The fold test, carried out on samples collected In the nearby section of Titjuschin where the sediments are exposed in a fold structure, indicates that the characteristic magnetization pre-dates the foldingSe presenta el perfil magnetoestratigráflco del Tatariense (Pérm...
International audienceWe present the magnetostratigraphy of the Abadeh section (central Iran). Therm...
International audienceWe present the magnetostratigraphy of the Abadeh section (central Iran). Therm...
International audienceWe have obtained new magnetostratigraphic results from two Precambrian sedimen...
The Late Permian is characterized palaeomagnetically by the transition from the long-lasting Permo-C...
The Late Permian is characterized palaeomagnetically by the transition from the long-lasting Permo-C...
The Late Permian is characterized palaeomagnetically by the transition from the long-lasting Permo-C...
A total of 297 samples for palaeomagnetic studies were collected from Upper Gzhelian through Spathia...
During the last five years there has been considerable doubt over the age of the continental uppermo...
© 2020 Kazan Federal University. All rights reserved. The results of a detailed paleomagnetic study ...
We present a reconnaissance paleomagnetic study of rocks from several formations of the Chita region...
We present a reconnaissance paleomagnetic study of rocks from several formations of the Chita region...
We present a reconnaissance paleomagnetic study of rocks from several formations of the Chita region...
International audienceWe present the magnetostratigraphy of the early Palaeozoic Moyero river sectio...
International audienceWe present the magnetostratigraphy of the early Palaeozoic Moyero river sectio...
© 2018 The Author(s). The reverse polarity Kiaman Superchron has strong evidence for at least three,...
International audienceWe present the magnetostratigraphy of the Abadeh section (central Iran). Therm...
International audienceWe present the magnetostratigraphy of the Abadeh section (central Iran). Therm...
International audienceWe have obtained new magnetostratigraphic results from two Precambrian sedimen...
The Late Permian is characterized palaeomagnetically by the transition from the long-lasting Permo-C...
The Late Permian is characterized palaeomagnetically by the transition from the long-lasting Permo-C...
The Late Permian is characterized palaeomagnetically by the transition from the long-lasting Permo-C...
A total of 297 samples for palaeomagnetic studies were collected from Upper Gzhelian through Spathia...
During the last five years there has been considerable doubt over the age of the continental uppermo...
© 2020 Kazan Federal University. All rights reserved. The results of a detailed paleomagnetic study ...
We present a reconnaissance paleomagnetic study of rocks from several formations of the Chita region...
We present a reconnaissance paleomagnetic study of rocks from several formations of the Chita region...
We present a reconnaissance paleomagnetic study of rocks from several formations of the Chita region...
International audienceWe present the magnetostratigraphy of the early Palaeozoic Moyero river sectio...
International audienceWe present the magnetostratigraphy of the early Palaeozoic Moyero river sectio...
© 2018 The Author(s). The reverse polarity Kiaman Superchron has strong evidence for at least three,...
International audienceWe present the magnetostratigraphy of the Abadeh section (central Iran). Therm...
International audienceWe present the magnetostratigraphy of the Abadeh section (central Iran). Therm...
International audienceWe have obtained new magnetostratigraphic results from two Precambrian sedimen...