Main Crater

Results: 18



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146th Lunar and Planetary Science Conferencepdf NEW INSIGHTS INTO THE MARTIAN LATE HEAVY BOMBARDMENT W.F. Bottke1, S. Marchi1, D. Vokrouhlicky1,2, S. Robbins1, B. Hynek3, and A. Morbidelli1,4. 1Southwest Res

46th Lunar and Planetary Science Conferencepdf NEW INSIGHTS INTO THE MARTIAN LATE HEAVY BOMBARDMENT W.F. Bottke1, S. Marchi1, D. Vokrouhlicky1,2, S. Robbins1, B. Hynek3, and A. Morbidelli1,4. 1Southwest Res

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Source URL: about.sjrdesign.net

Language: English - Date: 2015-01-26 22:42:37
2Brazos River, Texas: Drilling the K-T and Chicxulub Event Strata Gerta Keller Princeton University Project Objectives The main objective of this project was to drill the Cretaceus-Tertiary (K-T) transition in the Brazos

Brazos River, Texas: Drilling the K-T and Chicxulub Event Strata Gerta Keller Princeton University Project Objectives The main objective of this project was to drill the Cretaceus-Tertiary (K-T) transition in the Brazos

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Source URL: www.dosecc.org

Language: English - Date: 2010-06-21 15:17:18
3nanodivides. Nevertheless, close examination will reveal either residual or immaturely formed nanodivides. Furthermore, in all cases observed, the nanopeaks are arranged linearly. The ultrastructures of the abapical spin

nanodivides. Nevertheless, close examination will reveal either residual or immaturely formed nanodivides. Furthermore, in all cases observed, the nanopeaks are arranged linearly. The ultrastructures of the abapical spin

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Language: English - Date: 2011-05-06 03:37:14
4believe they are related to the depth, energy release, and mechanism of various types of eruptions that are transitional between the two end members, that is, between less violent gas emissions (roar, without explosive o

believe they are related to the depth, energy release, and mechanism of various types of eruptions that are transitional between the two end members, that is, between less violent gas emissions (roar, without explosive o

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Language: English - Date: 2011-05-06 05:43:08
5years. The lowering of the level may be equivalent to the amount of material ejected by the small strombolian eruptions. A deformation survey pattern set up in December 1980 was remeasured in December 1981; preliminary d

years. The lowering of the level may be equivalent to the amount of material ejected by the small strombolian eruptions. A deformation survey pattern set up in December 1980 was remeasured in December 1981; preliminary d

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Language: English - Date: 2011-05-06 05:43:14
6Volcanic activity of Mount Erebus, PHILIP R. KYLE* Institute of Polar Studies The Ohio State University

Volcanic activity of Mount Erebus, PHILIP R. KYLE* Institute of Polar Studies The Ohio State University

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Language: English - Date: 2011-05-06 06:13:27
7Seismicity of Mount Erebus and vicinity, J. KIENLE Geophysical Institute

Seismicity of Mount Erebus and vicinity, J. KIENLE Geophysical Institute

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Language: English - Date: 2011-05-06 04:08:10
8Bookman Old Style Negreta

Bookman Old Style Negreta

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Language: English - Date: 2011-05-06 18:15:46
9tients of the physical property contrasts for the inferred sources to facilitate further geologic investigation and modeling. This research was supported by National Science Foundation grant DDPReferences

tients of the physical property contrasts for the inferred sources to facilitate further geologic investigation and modeling. This research was supported by National Science Foundation grant DDPReferences

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Language: English - Date: 2011-05-06 18:13:08
10solutions indicate that the distribution of hypocentral depths is well controlled; hence, activity is concentrated in a region beneath the lava lake extending down to about sea level. Some events occur deeper. The pipeli

solutions indicate that the distribution of hypocentral depths is well controlled; hence, activity is concentrated in a region beneath the lava lake extending down to about sea level. Some events occur deeper. The pipeli

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Language: English - Date: 2011-05-06 18:15:14