1993
DOI: 10.1016/0037-0738(93)90004-o
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The influence of half-graben syn-depositional tilting on thickness variation and seam splitting in the Brunner Coal Measures, New Zealand

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Cited by 16 publications
(10 citation statements)
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“…Haszeldine and Anderton (1980) proposed periodic tectonic rise in the source area, which led to spreading of channels of braided rivers across the flat protected coastal plain. Titheridge (1993) describes syn-depositional fault activity and deposition of such deposits within individual blocks of half-grabens. According to Nemec (1992) coal deposition in the environments of the braided rivers and coastal plains is connected with relatively high water level, when the floodplain is flooded, which could be related to sea-level changes.…”
Section: Facies Associationmentioning
confidence: 99%
“…Haszeldine and Anderton (1980) proposed periodic tectonic rise in the source area, which led to spreading of channels of braided rivers across the flat protected coastal plain. Titheridge (1993) describes syn-depositional fault activity and deposition of such deposits within individual blocks of half-grabens. According to Nemec (1992) coal deposition in the environments of the braided rivers and coastal plains is connected with relatively high water level, when the floodplain is flooded, which could be related to sea-level changes.…”
Section: Facies Associationmentioning
confidence: 99%
“…The structural maps of Barry & MacFarlan (1988) and unpublished maps by Coalcorp have been compiled from the interpretation of aerial photographs, field mapping, and from mine plans. Three series of faults are recognised and mapped by Barry & MacFarlan (1988) (Titheridge 1988). The reverse faults truncate normal faults (e.g., the Mt William Fault truncates the Kelly Fault), indicating that movement on these reverse faults is younger.…”
Section: Faultsmentioning
confidence: 99%
“…The geology of this area has been mapped at 1:250 000 scale by Bowen (1964) and has been the subject of structural studies by Cave (1983a, b, c), coal geology and structural mapping by Barry & MacFarlan (1988), and sedimentological studies by Titheridge (1988). There is good coverage of the Buller Coalfield by high quality aerial photographs, and these have been used to produce orthophotos of selected areas (Department of Lands & Survey 1984, from which faults and joints can be recognised and accurately measured (see below).…”
Section: Introductionmentioning
confidence: 99%
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“…Coal deposits at Sullivan Mine are contained within the Brunner Coal Measures (BCM), which outcrop in uplifted blocks around the West Coast and Northern Westland area of New Zealand (Flores & Sykes 1996). The BCM are of Eocene age, are typically 30 to 100 m thick, and are composed of transgressive sandstonedominated sequences that also contain carbonaceous mudstones, conglomerates and shales (Titheridge 1992).…”
Section: Sullivan Minementioning
confidence: 99%