Chemical Composition of Rocks and Soils at the Pathfinder Site
Abstract As Viking Landers did not measure rock compositions, Pathfinder (PF) data are the first in this respect. This review gives no proof yet whether the PF rocks are igneous or sedimentary, but for petrogenetic reasons they could be igneous. We suggest a model in which Mars is covered by about 5...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Wänke, H. [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2001 |
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| Schlagwörter: |
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| Anmerkung: |
© Kluwer Academic Publishers 2001 |
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| Übergeordnetes Werk: |
Enthalten in: Space science reviews - Kluwer Academic Publishers, 1962, 96(2001), 1-4 vom: Apr., Seite 317-330 |
|---|---|
| Übergeordnetes Werk: |
volume:96 ; year:2001 ; number:1-4 ; month:04 ; pages:317-330 |
| Links: |
|---|
| DOI / URN: |
10.1023/A:1011961725645 |
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OLC203368539X |
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| 520 | |a Abstract As Viking Landers did not measure rock compositions, Pathfinder (PF) data are the first in this respect. This review gives no proof yet whether the PF rocks are igneous or sedimentary, but for petrogenetic reasons they could be igneous. We suggest a model in which Mars is covered by about 50% basaltic and 50% andesitic igneous rocks. The soils are a mixture of the two with addition of Mg-sulfate and -chloride plus iron compounds possibly derived from the hematite deposits. | ||
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10.1023/A:1011961725645 doi (DE-627)OLC203368539X (DE-He213)A:1011961725645-p DE-627 ger DE-627 rakwb eng 600 VZ 16,12 ssgn Wänke, H. verfasserin aut Chemical Composition of Rocks and Soils at the Pathfinder Site 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 2001 Abstract As Viking Landers did not measure rock compositions, Pathfinder (PF) data are the first in this respect. This review gives no proof yet whether the PF rocks are igneous or sedimentary, but for petrogenetic reasons they could be igneous. We suggest a model in which Mars is covered by about 50% basaltic and 50% andesitic igneous rocks. The soils are a mixture of the two with addition of Mg-sulfate and -chloride plus iron compounds possibly derived from the hematite deposits. Iron Chloride Hematite Igneous Rock Iron Compound Brückner, J. aut Dreibus, G. aut Rieder, R. aut Ryabchikov, I. aut Enthalten in Space science reviews Kluwer Academic Publishers, 1962 96(2001), 1-4 vom: Apr., Seite 317-330 (DE-627)129086606 (DE-600)4860-4 (DE-576)014420724 0038-6308 nnns volume:96 year:2001 number:1-4 month:04 pages:317-330 https://doi.org/10.1023/A:1011961725645 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-AST SSG-OPC-AST GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_2002 GBV_ILN_2279 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4306 GBV_ILN_4700 AR 96 2001 1-4 04 317-330 |
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Chemical Composition of Rocks and Soils at the Pathfinder Site |
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Abstract As Viking Landers did not measure rock compositions, Pathfinder (PF) data are the first in this respect. This review gives no proof yet whether the PF rocks are igneous or sedimentary, but for petrogenetic reasons they could be igneous. We suggest a model in which Mars is covered by about 50% basaltic and 50% andesitic igneous rocks. The soils are a mixture of the two with addition of Mg-sulfate and -chloride plus iron compounds possibly derived from the hematite deposits. © Kluwer Academic Publishers 2001 |
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Abstract As Viking Landers did not measure rock compositions, Pathfinder (PF) data are the first in this respect. This review gives no proof yet whether the PF rocks are igneous or sedimentary, but for petrogenetic reasons they could be igneous. We suggest a model in which Mars is covered by about 50% basaltic and 50% andesitic igneous rocks. The soils are a mixture of the two with addition of Mg-sulfate and -chloride plus iron compounds possibly derived from the hematite deposits. © Kluwer Academic Publishers 2001 |
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Abstract As Viking Landers did not measure rock compositions, Pathfinder (PF) data are the first in this respect. This review gives no proof yet whether the PF rocks are igneous or sedimentary, but for petrogenetic reasons they could be igneous. We suggest a model in which Mars is covered by about 50% basaltic and 50% andesitic igneous rocks. The soils are a mixture of the two with addition of Mg-sulfate and -chloride plus iron compounds possibly derived from the hematite deposits. © Kluwer Academic Publishers 2001 |
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Chemical Composition of Rocks and Soils at the Pathfinder Site |
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