Lithology and subdivisions of the jurassic stump formation in southeastern Idaho and adjoining areas: marked rapid lateral changes in lithology, fossil content, and thickness of the Stump Formation are due principally to erosion associated with the Cretaceous (K) and Jurassic (J-4) unconformities
Gespeichert in:
| Hauptverfasser: | , |
|---|---|
| Format: | Buch |
| Sprache: | English |
| Veröffentlicht: |
Washington
US Gov. Print. Off.
1979
|
| Schriftenreihe: | Geological Survey professional paper
1035-C Unconformities, correlation, and nomenclature of some triassic and Jurassic rocks, western interior United States |
| Beschreibung: | III, 25 S. Ill., graph. Darst., Kt. |
Internformat
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| 100 | 1 | |a Pipiringos, George N. |e Verfasser |4 aut | |
| 245 | 1 | 0 | |a Lithology and subdivisions of the jurassic stump formation in southeastern Idaho and adjoining areas |b marked rapid lateral changes in lithology, fossil content, and thickness of the Stump Formation are due principally to erosion associated with the Cretaceous (K) and Jurassic (J-4) unconformities |c by George N. Pipiringos and Ralph W. Imlay |
| 264 | 1 | |a Washington |b US Gov. Print. Off. |c 1979 | |
| 300 | |a III, 25 S. |b Ill., graph. Darst., Kt. | ||
| 336 | |b txt |2 rdacontent | ||
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| 490 | 1 | |a Geological Survey professional paper |v 1035-C | |
| 490 | 0 | |a Unconformities, correlation, and nomenclature of some triassic and Jurassic rocks, western interior United States | |
| 700 | 1 | |a Imlay, Ralph W. |e Verfasser |4 aut | |
| 810 | 2 | |a United States Geological Survey |t Professional paper |v 1035-C |w (DE-604)BV000005472 |9 1035-C | |
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Datensatz im Suchindex
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| author | Pipiringos, George N. Imlay, Ralph W. |
| author_facet | Pipiringos, George N. Imlay, Ralph W. |
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| id | DE-604.BV041900502 |
| illustrated | Illustrated |
| indexdate | 2024-07-10T01:07:49Z |
| institution | BVB |
| language | English |
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| physical | III, 25 S. Ill., graph. Darst., Kt. |
| publishDate | 1979 |
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| series2 | Geological Survey professional paper Unconformities, correlation, and nomenclature of some triassic and Jurassic rocks, western interior United States |
| spelling | Pipiringos, George N. Verfasser aut Lithology and subdivisions of the jurassic stump formation in southeastern Idaho and adjoining areas marked rapid lateral changes in lithology, fossil content, and thickness of the Stump Formation are due principally to erosion associated with the Cretaceous (K) and Jurassic (J-4) unconformities by George N. Pipiringos and Ralph W. Imlay Washington US Gov. Print. Off. 1979 III, 25 S. Ill., graph. Darst., Kt. txt rdacontent n rdamedia nc rdacarrier Geological Survey professional paper 1035-C Unconformities, correlation, and nomenclature of some triassic and Jurassic rocks, western interior United States Imlay, Ralph W. Verfasser aut United States Geological Survey Professional paper 1035-C (DE-604)BV000005472 1035-C |
| spellingShingle | Pipiringos, George N. Imlay, Ralph W. Lithology and subdivisions of the jurassic stump formation in southeastern Idaho and adjoining areas marked rapid lateral changes in lithology, fossil content, and thickness of the Stump Formation are due principally to erosion associated with the Cretaceous (K) and Jurassic (J-4) unconformities |
| title | Lithology and subdivisions of the jurassic stump formation in southeastern Idaho and adjoining areas marked rapid lateral changes in lithology, fossil content, and thickness of the Stump Formation are due principally to erosion associated with the Cretaceous (K) and Jurassic (J-4) unconformities |
| title_auth | Lithology and subdivisions of the jurassic stump formation in southeastern Idaho and adjoining areas marked rapid lateral changes in lithology, fossil content, and thickness of the Stump Formation are due principally to erosion associated with the Cretaceous (K) and Jurassic (J-4) unconformities |
| title_exact_search | Lithology and subdivisions of the jurassic stump formation in southeastern Idaho and adjoining areas marked rapid lateral changes in lithology, fossil content, and thickness of the Stump Formation are due principally to erosion associated with the Cretaceous (K) and Jurassic (J-4) unconformities |
| title_full | Lithology and subdivisions of the jurassic stump formation in southeastern Idaho and adjoining areas marked rapid lateral changes in lithology, fossil content, and thickness of the Stump Formation are due principally to erosion associated with the Cretaceous (K) and Jurassic (J-4) unconformities by George N. Pipiringos and Ralph W. Imlay |
| title_fullStr | Lithology and subdivisions of the jurassic stump formation in southeastern Idaho and adjoining areas marked rapid lateral changes in lithology, fossil content, and thickness of the Stump Formation are due principally to erosion associated with the Cretaceous (K) and Jurassic (J-4) unconformities by George N. Pipiringos and Ralph W. Imlay |
| title_full_unstemmed | Lithology and subdivisions of the jurassic stump formation in southeastern Idaho and adjoining areas marked rapid lateral changes in lithology, fossil content, and thickness of the Stump Formation are due principally to erosion associated with the Cretaceous (K) and Jurassic (J-4) unconformities by George N. Pipiringos and Ralph W. Imlay |
| title_short | Lithology and subdivisions of the jurassic stump formation in southeastern Idaho and adjoining areas |
| title_sort | lithology and subdivisions of the jurassic stump formation in southeastern idaho and adjoining areas marked rapid lateral changes in lithology fossil content and thickness of the stump formation are due principally to erosion associated with the cretaceous k and jurassic j 4 unconformities |
| title_sub | marked rapid lateral changes in lithology, fossil content, and thickness of the Stump Formation are due principally to erosion associated with the Cretaceous (K) and Jurassic (J-4) unconformities |
| volume_link | (DE-604)BV000005472 |
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