Caledonian tectonics from stratigraphy and isotope geochemistry of lower palaeozoic successions
<p>The Southern Uplands of Scotland is interpreted as a Lower Palaeozoic accretionary complex which formed on the northern margin of the Iapetus Ocean. Seven conglomerates which contain detritus derived from the north-west, from sources on the Laurentian continental margin, were studied. Gran...
| Príomhchruthaitheoirí: | , |
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| Formáid: | Tráchtas |
| Teanga: | English |
| Foilsithe / Cruthaithe: |
1987
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