Ewan M Campbell
Biographic Data
| ID | 5671160 |
|---|---|
| NAME | Ewan M Campbell |
| GIVEN NAMES | Ewan M |
| FAMILY NAME | Campbell |
| SIGNATURE | CAMPBELL E M |
| AFFILIATIONS | The University of Adelaide |
| ORCID | 0000-0002-5573-8243 |
| VERIFIED | Yes |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 4 |
| WORKS AS AUTHOR | 3 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1988 |
| LATEST PUBLICATION YEAR | 1991 |
| H-INDEX | 1 |
The early Cretaceous marine transgression and its significance for landscape interpretation
Significant elements of the Australian landscape date from Mesozoic or earlier times. Australia did not separate completely from other Gondwanan components until Early Tertiary times and these Mesozoic and older elements can therefore be regarded as Gondwanan. During the separation and northern drift of the continent and particularly in Late Jurassic and earlier Cretaceous times the sea invaded and spread across much of the erstwhile landmass. Th…
The gawler ranges, South Australia
The volcanic residuals of the Gawler Ranges together form an extensive massif that in its gross morphology differs markedly from most exposures of silicic volcanic rocks. The upland developed in two stages, the first involving differential fracture‐controlled subsurface weathering, the second the stripping of the regolith. As a result, an irregular weathering front was exposed, with domical projections prominent. These bornhardts are etch forms, …
Ancient Australia
Ancient Australia
The gawler ranges, South Australia
The volcanic residuals of the Gawler Ranges together form an extensive massif that in its gross morphology differs markedly from most exposures of silicic volcanic rocks. The upland developed in two stages, the first involving differential fracture‐controlled subsurface weathering, the second the stripping of the regolith. As a result, an irregular weathering front was exposed, with domical projections prominent. These bornhardts are etch forms, …
Ancient Australia
The early Cretaceous marine transgression and its significance for landscape interpretation
Significant elements of the Australian landscape date from Mesozoic or earlier times. Australia did not separate completely from other Gondwanan components until Early Tertiary times and these Mesozoic and older elements can therefore be regarded as Gondwanan. During the separation and northern drift of the continent and particularly in Late Jurassic and earlier Cretaceous times the sea invaded and spread across much of the erstwhile landmass. Th…
The gawler ranges, South Australia
The volcanic residuals of the Gawler Ranges together form an extensive massif that in its gross morphology differs markedly from most exposures of silicic volcanic rocks. The upland developed in two stages, the first involving differential fracture‐controlled subsurface weathering, the second the stripping of the regolith. As a result, an irregular weathering front was exposed, with domical projections prominent. These bornhardts are etch forms, …
Geology (3 works) · Paleontology (3 works) · Cretaceous (2 works) · Geography (2 works) · Geological and Geophysical Studies (2 works) · Geological formations and processes (2 works) · Geology (2 works) · Mesozoic (2 works) · Paleontology (2 works) · Structural basin (2 works)