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Creator |
bd12e480200a0e58504d6106bfed3c8a |
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Creator |
ext-7bf6b7e8db52ac199dfcbb4d48d7b44e |
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Date |
2011-03 |
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Is Part Of |
repository |
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abstract |
Home Plate is a plateau in the Columbia Hills of Gusev Crater. It is a layered sequence
of clastic rocks with alkali basaltic composition. Based on stratigraphy, structure,
sedimentology, mineralogy, and bulk chemistry it is interpreted as pyroclastic deposit
and thought to be extensively hydrothermally altered. The hydrothermal alteration
is presumed to be of high and low temperature nature. In order to better understand
the conditions (P,T,X) of hydrothermal alteration for the Home Plate region we have
calculated the hydrothermal alteration mineralogy of Fastball, a primitive basalt
from the Home Plate sequence, and compared these results to the mineralogy of the
area. |
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authorList |
authors |
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presentedAt |
ext-140c29de5896bcc818f22c174b664945 |
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status |
nonPeerReviewed |
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type |
AcademicArticle |
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type |
Article |
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label |
Filiberto, Justin and Schwenzer, Susanne (2011). Hydrothermal alteration mineralogy
of Home Plate: thermochemical contstraints for their formation conditions. In: 42nd
Lunar and Planetary Science Conference, 7-11 Mar 2011, Houston, TX, USA. |
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label |
Filiberto, Justin and Schwenzer, Susanne (2011). Hydrothermal alteration mineralogy
of Home Plate: thermochemical contstraints for their formation conditions. In: 42nd
Lunar and Planetary Science Conference, 7-11 Mar 2011, Houston, TX, USA. |
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Title |
Hydrothermal alteration mineralogy of Home Plate: thermochemical contstraints for
their formation conditions |
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in dataset |
oro |