Bumi Bola Salju (Indonesian Wikipedia)

Analysis of information sources in references of the Wikipedia article "Bumi Bola Salju" in Indonesian language version.

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13doi.org

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6harvard.edu

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2toolserver.org

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2wikipedia.org

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2nih.gov

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2geoscienceworld.org

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1caltech.edu

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1princeton.edu

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1igcp512.com

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1web.archive.org

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1sciencemag.org

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1sciencedaily.com

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1springerlink.com

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1pnas.org

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caltech.edu

gps.caltech.edu

Kirschvink, J.L. (1992). "Late Proterozoic low-latitude global glaciation: The snowball Earth". Dalam Schopf, JW, and Klein, C. The Proterozoic Biosphere: A Multidisciplinary Study (PDF). Cambridge University Press. hlm. 51–2.

doi.org

Allen, Philip A.; Etienne, James L. (2008). "Sedimentary challenge to Snowball Earth". Nature Geoscience. 1 (12): 817. doi:10.1038/ngeo355.
W. B. Harland (1964). "Critical evidence for a great infra-Cambrian glaciation". International Journal of Earth Sciences. 54 (1): 45–61. Bibcode:1964GeoRu..54...45H. doi:10.1007/BF01821169.
M.I. Budyko (1969). "Effect of solar radiation variation on climate of Earth". Tellus A. 21 (5): 611–1969. doi:10.1111/j.2153-3490.1969.tb00466.x.
Harland, W.B. (1964). "Critical evidence for a great infra-Cambrian glaciation" (PDF). International Journal of Earth Sciences. 54 (1): 45–61. Bibcode:1964GeoRu..54...45H. doi:10.1007/BF01821169. Diakses tanggal 11 March 2008. ^{[pranala nonaktif permanen]}
Budyko, M.I. (1969). "The effect of solar radiation variations on the climate of the earth". Tellus. 21 (5): 611–9. doi:10.1111/j.2153-3490.1969.tb00466.x.
D.A.D. Evans (2000). "Stratigraphic, geochronological, and palaeomagnetic constraints upon the Neoproterozoic climatic paradox". American Journal of Science. 300 (5): 347–433. doi:10.2475/ajs.300.5.347.
Young, G.M. (1 February 1995). "Are Neoproterozoic glacial deposits preserved on the margins of Laurentia related to the fragmentation of two supercontinents?". Geology. 23 (2): 153–6. Bibcode:1995Geo....23..153Y. doi:10.1130/0091-7613(1995)023<0153:ANGDPO>2.3.CO;2. Diakses tanggal 27 April 2007.
Sohl, L.E. (1999). "Paleomagnetic polarity reversals in Marinoan (ca. 600 Ma) glacial deposits of Australia; implications for the duration of low-latitude glaciation in Neoproterozoic time". Bulletin of the Geological Society of America. 111 (8): 1120–39. Bibcode:1999GSAB..111.1120S. doi:10.1130/0016-7606(1999)111<1120:PPRIMC>2.3.CO;2. Diakses tanggal 11 March 2008.
Arnaud, E. (2002). "Glacial influence on Neoproterozoic sedimentation: the Smalfjord Formation, northern Norway". Sedimentology. 49 (4): 765–88. doi:10.1046/j.1365-3091.2002.00466.x.
D.H. Rothman; J.M. Hayes; R.E. Summons (2003). "Dynamics of the Neoproterozoic carbon cycle". Proc. Natl. Acad. Sci. U.S.A. 100 (14): 124–9. Bibcode:2003PNAS..100.8124R. doi:10.1073/pnas.0832439100. PMC 166193 . PMID 12824461.
Kaufman, Alan J. (24 June 1997). "Isotopes, ice ages, and terminal Proterozoic earth history". Proc. Natl. Acad. Sci. U.S.A. 94 (13): 6600–5. Bibcode:1997PNAS...94.6600K. doi:10.1073/pnas.94.13.6600. PMC 21204 . PMID 11038552. Diakses tanggal 6 May 2007.

dx.doi.org

DOI:10.1098/rsbm.1960.0011
Rujukan ini akan diselesaikan secara otomatis dalam beberapa menit. Anda dapat melewati antrian atau membuat secara manual
DOI:10.1126/science.281.5381.1342 10.1126/science.281.5381.1342
Rujukan ini akan diselesaikan secara otomatis dalam beberapa menit. Anda dapat melewati antrian atau membuat secara manual

geoscienceworld.org

geology.geoscienceworld.org

Young, G.M. (1 February 1995). "Are Neoproterozoic glacial deposits preserved on the margins of Laurentia related to the fragmentation of two supercontinents?". Geology. 23 (2): 153–6. Bibcode:1995Geo....23..153Y. doi:10.1130/0091-7613(1995)023<0153:ANGDPO>2.3.CO;2. Diakses tanggal 27 April 2007.

bulletin.geoscienceworld.org

Sohl, L.E. (1999). "Paleomagnetic polarity reversals in Marinoan (ca. 600 Ma) glacial deposits of Australia; implications for the duration of low-latitude glaciation in Neoproterozoic time". Bulletin of the Geological Society of America. 111 (8): 1120–39. Bibcode:1999GSAB..111.1120S. doi:10.1130/0016-7606(1999)111<1120:PPRIMC>2.3.CO;2. Diakses tanggal 11 March 2008.

harvard.edu

adsabs.harvard.edu

W. B. Harland (1964). "Critical evidence for a great infra-Cambrian glaciation". International Journal of Earth Sciences. 54 (1): 45–61. Bibcode:1964GeoRu..54...45H. doi:10.1007/BF01821169.
Harland, W.B. (1964). "Critical evidence for a great infra-Cambrian glaciation" (PDF). International Journal of Earth Sciences. 54 (1): 45–61. Bibcode:1964GeoRu..54...45H. doi:10.1007/BF01821169. Diakses tanggal 11 March 2008. ^{[pranala nonaktif permanen]}
Young, G.M. (1 February 1995). "Are Neoproterozoic glacial deposits preserved on the margins of Laurentia related to the fragmentation of two supercontinents?". Geology. 23 (2): 153–6. Bibcode:1995Geo....23..153Y. doi:10.1130/0091-7613(1995)023<0153:ANGDPO>2.3.CO;2. Diakses tanggal 27 April 2007.
Sohl, L.E. (1999). "Paleomagnetic polarity reversals in Marinoan (ca. 600 Ma) glacial deposits of Australia; implications for the duration of low-latitude glaciation in Neoproterozoic time". Bulletin of the Geological Society of America. 111 (8): 1120–39. Bibcode:1999GSAB..111.1120S. doi:10.1130/0016-7606(1999)111<1120:PPRIMC>2.3.CO;2. Diakses tanggal 11 March 2008.
D.H. Rothman; J.M. Hayes; R.E. Summons (2003). "Dynamics of the Neoproterozoic carbon cycle". Proc. Natl. Acad. Sci. U.S.A. 100 (14): 124–9. Bibcode:2003PNAS..100.8124R. doi:10.1073/pnas.0832439100. PMC 166193 . PMID 12824461.
Kaufman, Alan J. (24 June 1997). "Isotopes, ice ages, and terminal Proterozoic earth history". Proc. Natl. Acad. Sci. U.S.A. 94 (13): 6600–5. Bibcode:1997PNAS...94.6600K. doi:10.1073/pnas.94.13.6600. PMC 21204 . PMID 11038552. Diakses tanggal 6 May 2007.

igcp512.com

Detailed information on International Geoscience Programme (IGCP) Project 512: Neoproterozoic Ice Ages can be found at http://www.igcp512.com/ Diarsipkan 2007-04-22 di Wayback Machine.

nih.gov

ncbi.nlm.nih.gov

D.H. Rothman; J.M. Hayes; R.E. Summons (2003). "Dynamics of the Neoproterozoic carbon cycle". Proc. Natl. Acad. Sci. U.S.A. 100 (14): 124–9. Bibcode:2003PNAS..100.8124R. doi:10.1073/pnas.0832439100. PMC 166193 . PMID 12824461.
Kaufman, Alan J. (24 June 1997). "Isotopes, ice ages, and terminal Proterozoic earth history". Proc. Natl. Acad. Sci. U.S.A. 94 (13): 6600–5. Bibcode:1997PNAS...94.6600K. doi:10.1073/pnas.94.13.6600. PMC 21204 . PMID 11038552. Diakses tanggal 6 May 2007.

pnas.org

Kaufman, Alan J. (24 June 1997). "Isotopes, ice ages, and terminal Proterozoic earth history". Proc. Natl. Acad. Sci. U.S.A. 94 (13): 6600–5. Bibcode:1997PNAS...94.6600K. doi:10.1073/pnas.94.13.6600. PMC 21204 . PMID 11038552. Diakses tanggal 6 May 2007.

princeton.edu

Princeton University - Franklyn Van Houten, expert on sedimentary rocks, dies at 96

sciencedaily.com

Snowball Earth: New Evidence Hints at Global Glaciation 716.5 Million Years Ago Geologists have found evidence that sea ice extended to the equator 716.5 million years ago. 5 March 2010.

sciencemag.org

Calibrating the Cryogenian, Abstract only: "Ice ... implies that the Sturtian glaciation was global in extent". 5 March 2010.

springerlink.com

Harland, W.B. (1964). "Critical evidence for a great infra-Cambrian glaciation" (PDF). International Journal of Earth Sciences. 54 (1): 45–61. Bibcode:1964GeoRu..54...45H. doi:10.1007/BF01821169. Diakses tanggal 11 March 2008. ^{[pranala nonaktif permanen]}

toolserver.org

DOI:10.1098/rsbm.1960.0011
Rujukan ini akan diselesaikan secara otomatis dalam beberapa menit. Anda dapat melewati antrian atau membuat secara manual
DOI:10.1126/science.281.5381.1342 10.1126/science.281.5381.1342
Rujukan ini akan diselesaikan secara otomatis dalam beberapa menit. Anda dapat melewati antrian atau membuat secara manual

web.archive.org

Detailed information on International Geoscience Programme (IGCP) Project 512: Neoproterozoic Ice Ages can be found at http://www.igcp512.com/ Diarsipkan 2007-04-22 di Wayback Machine.

wikipedia.org

id.wikipedia.org

DOI:10.1098/rsbm.1960.0011
Rujukan ini akan diselesaikan secara otomatis dalam beberapa menit. Anda dapat melewati antrian atau membuat secara manual
DOI:10.1126/science.281.5381.1342 10.1126/science.281.5381.1342
Rujukan ini akan diselesaikan secara otomatis dalam beberapa menit. Anda dapat melewati antrian atau membuat secara manual