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chair

koro

Last Update: 2014-06-09
Subject: General
Usage Frequency: 1
Quality:
Reference: Anonymous

Chair

Upuan

Last Update: 2014-10-01
Usage Frequency: 11
Quality:
Reference: Wikipedia

Chair

Salungpuwet

Last Update: 2013-10-10
Usage Frequency: 3
Quality:
Reference: Wikipedia

Chair

Silya

Last Update: 2013-08-25
Usage Frequency: 1
Quality:
Reference: Wikipedia

Chair

tayan atyan

Last Update: 2013-08-20
Usage Frequency: 1
Quality:
Reference: Anonymous

Chair

Pew

Last Update: 2013-08-19
Usage Frequency: 1
Quality:
Reference: Wikipedia

Chair

Salungki

Last Update: 2013-08-17
Usage Frequency: 1
Quality:
Reference: Wikipedia

Chair

Salungpuwit

Last Update: 2013-08-16
Usage Frequency: 1
Quality:
Reference: Wikipedia

Chair

Salong puwit

Last Update: 2013-07-27
Usage Frequency: 1
Quality:
Reference: Wikipedia

Chair

Salung-puwit

Last Update: 2013-07-03
Usage Frequency: 3
Quality:
Reference: Wikipedia

Chair

Salungpwet

Last Update: 2013-02-16
Subject: General
Usage Frequency: 1
Quality:

Chair

Bench

Last Update: 2011-08-16
Usage Frequency: 1
Quality:
Reference: Wikipedia

Wooden chair

Upuan

Last Update: 2013-08-07
Usage Frequency: 1
Quality:
Reference: Wikipedia

Rock music

Musikang rock

Last Update: 2014-10-07
Usage Frequency: 1
Quality:
Reference: Wikipedia

The transitional hydrosphere The nature of the rock record from the time of the first sedimentary rocks (approximately 3.8 billion years ago) to about one to two billion years ago suggests that the amount of oxygen in the Earth’s atmosphere was significantly lower than it is today and that there were continuous chemical trends in the sedimentary rocks formed and, more subtly, in the composition of the hydrosphere. The chemistry of rocks shifted dramatically during this transitional period. The source rocks of sediments during this time may have been more basaltic than subsequent ones. Sedimentary debris was formed by the alteration of such source rocks in an oxygen-deficient atmosphere and accumulated primarily under anaerobic marine conditions.

The transitional hydrosphere The nature of the rock record from the time of the first sedimentary rocks (approximately 3.8 billion years ago) to about one to two billion years ago suggests that the amount of oxygen in the Earth’s atmosphere was significantly lower than it is today and that there were continuous chemical trends in the sedimentary rocks formed and, more subtly, in the composition of the hydrosphere. The chemistry of rocks shifted dramatically during this transitional period. The source rocks of sediments during this time may have been more basaltic than subsequent ones. Sedimentary debris was formed by the alteration of such source rocks in an oxygen-deficient atmosphere and accumulated primarily under anaerobic marine conditions.

Last Update: 2014-09-23
Subject: General
Usage Frequency: 1
Quality:
Reference: Anonymous

sedimentary rock

rock nalatak

Last Update: 2014-09-22
Subject: General
Usage Frequency: 1
Quality:
Reference: Anonymous

gills rock

hasang bato

Last Update: 2014-09-01
Subject: General
Usage Frequency: 1
Quality:
Reference: Anonymous

Chairs

Upuan

Last Update: 2014-08-18
Usage Frequency: 1
Quality:
Reference: Wikipedia

You rocked my world

niyanig

Last Update: 2014-06-30
Subject: General
Usage Frequency: 1
Quality:
Reference: Anonymous

Rock

Rock

Last Update: 2014-06-27
Usage Frequency: 3
Quality:
Reference: Wikipedia

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