13 research outputs found
Π‘ΠΠΠ«Π’ΠΠΠΠΠ― Π‘Π’Π ΠΠ’ΠΠΠ ΠΠ€ΠΠ― Π ΠΠ ΠΠΠΠΠΠ« ΠΠΠ Π ΠΠΠ―Π¦ΠΠ ΠΠ ΠΠΠΠΠΠ‘ΠΠΠ₯ Π‘Π’Π ΠΠ’ΠΠΠΠ ΠΠΠ ΠΠΠΠ ΠΠΠ’ΠΠ― Π Π‘ΠΠΠΠΠ Π
Study of the Ordovician sedimentary sequences of Gorny Altai and Salair has revealed lithological and paleontological features correlating with global sedimentary events:(1) The Acerocare Regressive Event (an initial event in the Early Tremadocian);(2) Black Mountain Transgressive Event (Early Tremadocian);(3) Peltocare Regressive Event (Tremadocian);(4) Kelly Creek Regressive Event (Late Tremadocian);(5) Ceratopyge Regressive Event (Late Tremadocian);(6) Billingen Transgressive Event (Early Floian);(7) Stein Lowstand Event (Middle Darriwilian);(8) Vollen Lowstand Event (Sandbian);(9) Arestad Drowning Event (Middle Sandbian);(10) Frognerkilen Lowstand Event (Early Katian);(11) Linearis Drowning Events 1 and 2 (Middle Katian);(12) Terminal Husbergoya Lowstand Event (Hirnantian); and(13) Hirnantian Lowstand Event (HICE) (Late Ordovician).The chronostratigraphic levels with traces of the global sedimentary events in the Uymen-Lebed structural-facies zone (SFZ) (Gorny Altai) differ from those in the Charysh-Inya and Anui-Chuya SFZ (Altai). In the Ordovician, the Altai basin located in the Charysh-Inya and Anui-Chuya SFZ was a marine area separated from both the Uymen-Lebed basin and the coeval Salair basin. The traces of the global sedimentary and/or biotic events in the Altai and Salair sections can be used as a precise basis for direct correlation of the local stratigraphic units with the units of the International Stratigraphic Chart.Π ΠΎΡΠ΄ΠΎΠ²ΠΈΠΊΡΠΊΠΈΡ
ΠΎΡΠ°Π΄ΠΎΡΠ½ΡΡ
ΠΏΠΎΡΠ»Π΅Π΄ΠΎΠ²Π°ΡΠ΅Π»ΡΠ½ΠΎΡΡΡΡ
ΠΠΎΡΠ½ΠΎΠ³ΠΎ ΠΠ»ΡΠ°Ρ ΠΈ Π‘Π°Π»Π°ΠΈΡΠ° Π²ΡΠ΄Π΅Π»Π΅Π½Ρ Π»ΠΈΡΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΈ ΠΏΠ°Π»Π΅ΠΎΠ½ΡΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΎΡΠΎΠ±Π΅Π½Π½ΠΎΡΡΠΈ, ΠΊΠΎΡΠΎΡΡΠ΅ ΠΊΠΎΡΡΠ΅Π»ΠΈΡΡΡΡΡΡ Ρ Π³Π»ΠΎΠ±Π°Π»ΡΠ½ΡΠΌΠΈ ΡΠ΅Π΄ΠΈΠΌΠ΅Π½ΡΠ°ΡΠΈΠΎΠ½Π½ΡΠΌΠΈ ΡΠΎΠ±ΡΡΠΈΡΠΌΠΈ:1) ΠΈΠ½ΠΈΡΠΈΠ°Π»ΡΠ½ΡΠΌ ΡΠ°Π½Π½Π΅ΡΡΠ΅ΠΌΠ°Π΄ΠΎΠΊΡΠΊΠΈΠΌ ΡΠ΅Π³ΡΠ΅ΡΡΠΈΠ²Π½ΡΠΌ ΠΡΠ΅ΡΠΎΠΊΠ°ΡΠ΅ (Acerocare),2) ΡΠ°Π½Π½Π΅ΡΡΠ΅ΠΌΠ°Π΄ΠΎΠΊΡΠΊΠΈΠΌ ΡΡΠ°Π½ΡΠ³ΡΠ΅ΡΡΠΈΠ²Π½ΡΠΌ ΠΠ»ΡΠΊ ΠΠ°ΡΠ½ΡΠΈΠ½ (Black Mountain),3) ΡΡΠ΅ΠΌΠ°Π΄ΠΎΠΊΡΠΊΠΈΠΌ ΡΠ΅Π³ΡΠ΅ΡΡΠΈΠ²Π½ΡΠΌ ΠΠ΅Π»ΡΡΠΎΠΊΠ°ΡΠ΅ (Peltocare),4) ΠΏΠΎΠ·Π΄Π½Π΅ΡΡΠ΅ΠΌΠ°Π΄ΠΎΠΊΡΠΊΠΈΠΌ ΡΠ΅Π³ΡΠ΅ΡΡΠΈΠ²Π½ΡΠΌ ΠΠ΅Π»Π»ΠΈ ΠΡΠΈΠΊ (Kelly Creek),5) ΠΏΠΎΠ·Π΄Π½Π΅ΡΡΠ΅ΠΌΠ°Π΄ΠΎΠΊΡΠΊΠΈΠΌ ΡΠ΅Π³ΡΠ΅ΡΡΠΈΠ²Π½ΡΠΌ Π¦Π΅ΡΠ°ΡΠΎΠΏΠΈΠ³Π΅ (Ceratopyge),6) ΡΠ°Π½Π½Π΅ΡΠ»ΠΎΡΠΊΠΈΠΌ ΡΡΠ°Π½ΡΠ³ΡΠ΅ΡΡΠΈΠ²Π½ΡΠΌ ΠΠΈΠ»Π»ΠΈΠ½Π³Π΅Π½ (Billingen),7) ΡΡΠ΅Π΄Π½Π΅Π΄Π°ΡΡΠΈΠ²ΠΈΠ»ΡΡΠΊΠΈΠΌ ΡΠ΅Π³ΡΠ΅ΡΡΠΈΠ²Π½ΡΠΌ Π‘ΡΠ΅ΠΉΠ½ (Stein),8) ΡΠ°Π½Π½Π΅ΡΠ°Π½Π΄Π±ΠΈΠΉΡΠΊΠΈΠΌ ΡΠ΅Π³ΡΠ΅ΡΡΠΈΠ²Π½ΡΠΌ ΠΠΎΠ»Π»Π΅Π½ (Vollen Lowstand),9) ΡΡΠ΅Π΄Π½Π΅ΡΠ°Π½Π±ΠΈΠΉΡΠΊΠΈΠΌ ΡΡΠ°Π½ΡΠ³ΡΠ΅ΡΡΠΈΠ²Π½ΡΠΌ ΠΡΠΈΡΡΠ°Π΄ (Arestad),10) ΡΠ°Π½Π½Π΅ΠΊΠ°ΡΠΈΠΉΡΠΊΠΈΠΌ ΡΠ΅Π³ΡΠ΅ΡΡΠΈΠ²Π½ΡΠΌ Π€ΡΠΎΠ³Π½Π΅ΡΠΊΠΈΠ»Π΅Π½ (Frognerkilen),11) ΡΡΠ΅Π΄Π½Π΅ΠΊΠ°ΡΠΈΠΉΡΠΊΠΈΠΌ ΡΠ΅Π³ΡΠ΅ΡΡΠΈΠ²Π½ΡΠΌ ΠΠΈΠ½Π΅Π°ΡΠΈΡ (Linearis),12) Ρ
ΠΈΡΠ½Π°Π½ΡΡΠΊΠΈΠΌ ΡΠ΅Π³ΡΠ΅ΡΡΠΈΠ²Π½ΡΠΌ β Π’Π΅ΡΠΌΠΈΠ½Π°Π»ΡΠ½ΡΠΉ Π₯ΡΡΠ±Π΅ΡΠ³ΠΎΠΉΡ (Terminal Husbergoya),13) ΠΏΠΎΠ·Π΄Π½Π΅ΠΎΡΠ΄ΠΎΠ²ΠΈΠΊΡΠΊΠΈΠΌ ΡΠ΅Π³ΡΠ΅ΡΡΠΈΠ²Π½ΡΠΌ Π₯ΠΈΡΠ½Π°Π½Ρ (Hirnantian Lowstand) (HICE).Π₯ΡΠΎΠ½ΠΎΡΡΡΠ°ΡΠΈΠ³ΡΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΡΡΠΎΠ²Π½ΠΈ ΠΏΡΠΎΡΠ²Π»Π΅Π½ΠΈΡ ΡΠ»Π΅Π΄ΠΎΠ² Π³Π»ΠΎΠ±Π°Π»ΡΠ½ΡΡ
ΡΠ΅Π΄ΠΈΠΌΠ΅Π½ΡΠ°ΡΠΈΠΎΠ½Π½ΡΡ
ΡΠΎΠ±ΡΡΠΈΠΉ Π² Π£ΠΉΠΌΠ΅Π½ΡΠΊΠΎ-ΠΠ΅Π±Π΅Π΄ΡΠΊΠΎΠΉ ΡΡΡΡΠΊΡΡΡΠ½ΠΎ-ΡΠ°ΡΠΈΠ°Π»ΡΠ½ΠΎΠΉ Π·ΠΎΠ½Π΅ (Π‘Π€Π) ΠΠΎΡΠ½ΠΎΠ³ΠΎ ΠΠ»ΡΠ°Ρ ΠΎΡΠ»ΠΈΡΠ°ΡΡΡΡ ΠΎΡ ΡΡΠΎΠ²Π½Π΅ΠΉ ΠΏΡΠΎΡΠ²Π»Π΅Π½ΠΈΡ ΡΠ»Π΅Π΄ΠΎΠ² Π³Π»ΠΎΠ±Π°Π»ΡΠ½ΡΡ
ΡΠ΅Π΄ΠΈΠΌΠ΅Π½ΡΠ°ΡΠΈΠΎΠ½Π½ΡΡ
ΡΠΎΠ±ΡΡΠΈΠΉ Π² Π§Π°ΡΡΡΡΠΊΠΎ-ΠΠ½ΡΠΊΠΎΠΉ ΠΈ ΠΠ½ΡΠΉΡΠΊΠΎ-Π§ΡΠΉΡΠΊΠΎΠΉ Π‘Π€Π ΠΠ»ΡΠ°Ρ. ΠΠ»ΡΠ°ΠΉΡΠΊΠΈΠΉ ΠΎΡΠ΄ΠΎΠ²ΠΈΠΊΡΠΊΠΈΠΉ Π±Π°ΡΡΠ΅ΠΉΠ½, ΡΠ°ΡΠΏΠΎΠ»Π°Π³Π°Π²ΡΠΈΠΉΡΡ Π² Π§Π°ΡΡΡΡΠΊΠΎ-ΠΠ½ΡΠΊΠΎΠΉ ΠΈ ΠΠ½ΡΠΉΡΠΊΠΎ-Π§ΡΠΉΡΠΊΠΎΠΉ Π‘Π€Π, Π±ΡΠ» ΠΌΠΎΡΡΠΊΠΎΠΉ Π°ΠΊΠ²Π°ΡΠΎΡΠΈΠ΅ΠΉ, ΠΎΠ±ΠΎΡΠΎΠ±Π»Π΅Π½Π½ΠΎΠΉ ΠΊΠ°ΠΊ ΠΎΡ Π£ΠΉΠΌΠ΅Π½ΡΠΊΠΎ-ΠΠ΅Π±Π΅Π΄ΡΠΊΠΎΠ³ΠΎ, ΡΠ°ΠΊ ΠΈ ΠΎΡ Π‘Π°Π»Π°ΠΈΡΡΠΊΠΎΠ³ΠΎ ΠΎΠ΄Π½ΠΎΠ²ΠΎΠ·ΡΠ°ΡΡΠ½ΠΎΠ³ΠΎ Π±Π°ΡΡΠ΅ΠΉΠ½Π°. ΠΠ°ΡΠΈΠΊΡΠΈΡΠΎΠ²Π°Π½Π½ΡΠ΅ Π² Π°Π»ΡΠ°ΠΉΡΠΊΠΈΡ
ΠΈ ΡΠ°Π»Π°ΠΈΡΡΠΊΠΈΡ
ΡΠ°Π·ΡΠ΅Π·Π°Ρ
ΡΠ»Π΅Π΄Ρ Π³Π»ΠΎΠ±Π°Π»ΡΠ½ΡΡ
ΡΠ΅Π΄ΠΈΠΌΠ΅Π½ΡΠ°ΡΠΈΠΎΠ½Π½ΡΡ
ΠΈ (ΠΈΠ»ΠΈ) Π±ΠΈΠΎΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΠΎΠ±ΡΡΠΈΠΉ ΠΌΠΎΠ³ΡΡ ΡΠ»ΡΠΆΠΈΡΡ ΠΏΡΠ΅ΡΠΈΠ·ΠΈΠΎΠ½Π½ΠΎΠΉ ΠΎΡΠ½ΠΎΠ²ΠΎΠΉ Π΄Π»Ρ ΠΏΡΡΠΌΠΎΠΉ ΠΊΠΎΡΡΠ΅Π»ΡΡΠΈΠΈ ΠΌΠ΅ΡΡΠ½ΡΡ
ΡΡΡΠ°ΡΠΈΠ³ΡΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΏΠΎΠ΄ΡΠ°Π·Π΄Π΅Π»Π΅Π½ΠΈΠΉ Ρ ΡΡΡΡΠ½ΡΠΌΠΈ ΠΏΠΎΠ΄ΡΠ°Π·Π΄Π΅Π»Π΅Π½ΠΈΡΠΌΠΈ ΠΠ΅ΠΆΠ΄ΡΠ½Π°ΡΠΎΠ΄Π½ΠΎΠΉ ΡΡΡΠ°ΡΠΈΠ³ΡΠ°ΡΠΈΡΠ΅ΡΠΊΠΎΠΉ ΡΠΊΠ°Π»Ρ
Modern microwave methods in solid state inorganic materials chemistry: from fundamentals to manufacturing
No abstract available
EVENT STRATIGRAPHY AND CORRELATION PROBLEMS OF THE ORDOVICIAN STRATA OF GORNY ALTAI AND SALAIR
Study of the Ordovician sedimentary sequences of Gorny Altai and Salair has revealed lithological and paleontological features correlating with global sedimentary events:(1) The Acerocare Regressive Event (an initial event in the Early Tremadocian);(2) Black Mountain Transgressive Event (Early Tremadocian);(3) Peltocare Regressive Event (Tremadocian);(4) Kelly Creek Regressive Event (Late Tremadocian);(5) Ceratopyge Regressive Event (Late Tremadocian);(6) Billingen Transgressive Event (Early Floian);(7) Stein Lowstand Event (Middle Darriwilian);(8) Vollen Lowstand Event (Sandbian);(9) Arestad Drowning Event (Middle Sandbian);(10) Frognerkilen Lowstand Event (Early Katian);(11) Linearis Drowning Events 1 and 2 (Middle Katian);(12) Terminal Husbergoya Lowstand Event (Hirnantian); and(13) Hirnantian Lowstand Event (HICE) (Late Ordovician).The chronostratigraphic levels with traces of the global sedimentary events in the Uymen-Lebed structural-facies zone (SFZ) (Gorny Altai) differ from those in the Charysh-Inya and Anui-Chuya SFZ (Altai). In the Ordovician, the Altai basin located in the Charysh-Inya and Anui-Chuya SFZ was a marine area separated from both the Uymen-Lebed basin and the coeval Salair basin. The traces of the global sedimentary and/or biotic events in the Altai and Salair sections can be used as a precise basis for direct correlation of the local stratigraphic units with the units of the International Stratigraphic Chart