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New Zealand and Oblique‐Slip Margins: Tectonic Development up to and during the Cainozoic
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Publications
New Zealand and Oblique‐Slip Margins: Tectonic Development up to and during the Cainozoic
New Zealand and Oblique‐Slip Margins: Tectonic Development up to and during the Cainozoic
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K. B. Spörli
K. B. Spörli
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11 September 1980
book chapter
Published by
Wiley
p.
147-170
https://doi.org/10.1002/9781444303735.ch9
Abstract
No abstract available
Keywords
NEW ZEALAND AND OBLIQUE-SLIP MARGINS - TECTONIC DEVELOPMENT
OBLIQUE STRUCTURES
DEVELOPING DURING DEPOSITION AND DEFORMATION OF THE CARBONIFEROUS TO LATE JURASSIC RANGITATA SEQUENCE
OBLIQUE RHOMBIC PATTERNS
DOMINATING CAINOZOIC BLOCK FAULT SYSTEMS
HAWKE'S BAY AND WANGANUI MONOCLINES - TECTONIC FEATURES OF THE NORTH ISLAND
FAULTING
DOMINATING CAINOZOIC TECTONIC PATTERN
ALPINE FAULT
MAJOR TECTONIC FEATURE OF NEW ZEALAND
LATE CRETACEOUS-EARLY TERTIARY BASINS
CONSISTING OF TASMAN SEA BASIN
Cited by 36 articles