Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Mike R. Johnston"'
Publikováno v:
New Zealand Journal of Geology and Geophysics. 63:168-189
The Waimea-Flaxmore Fault System (W-FFS) comprises NE-striking, SE-dipping reverse faults superposing Eastern Province terranes on Cenozoic sedimentary units of the Moutere Depression. We p...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fdc9492b333696430ece0b39d7639e84
https://doi.org/10.1080/00288306.2019.1651346
https://doi.org/10.1080/00288306.2019.1651346
Publikováno v:
Geological Society, London, Memoirs. 49:1-14
This Memoir presents and discusses recent research mainly concerning the Permian and Triassic geological development of South Island in its regional context, which includes New Zealand as a whole, the continent of Zealandia, eastern Australia and Ant
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::471ab54d5a153f769dc4eeb49c48c20f
https://doi.org/10.1144/m49.7
https://doi.org/10.1144/m49.7
Publikováno v:
Geological Society, London, Memoirs. 49:331-372
The Western Province is a fragment of the c. 500 Ma SE Gondwana active continental margin. The Eastern Province is a terrane assemblage, which is partly stitched by the Median Batholith. Fragments of the batholith are preserved in the adjacent Drumdu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::97c5914aafb44338ff9fa52d1793457c
https://doi.org/10.1144/m49.8
https://doi.org/10.1144/m49.8
Autor:
Mike R. Johnston
Publikováno v:
Geological Society, London, Memoirs. 49:15-30
This chapter traces the history of understanding the central terranes of New Zealand: Drumduan, Brook Street, Murihiku, Dun Mountain–Maitai and Caples. The terranes, mostly exposed in the South Island, are named from stratigraphic units of Late Pal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7d8db359ad4c86ae0e1c78326692631e
https://doi.org/10.1144/m49.2
https://doi.org/10.1144/m49.2
Publikováno v:
New Zealand Journal of Geology and Geophysics. 61:461-479
The subsurface structure of the Moutere Depression is obscured by a thick Plio-Quaternary gravel sequence. Surface and subsurface data have been used to define a blind basement pop-up bounded to th...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::77404cadd799e8068d75c34a9ed94e88
https://doi.org/10.1080/00288306.2018.1502673
https://doi.org/10.1080/00288306.2018.1502673
Autor:
Kenneth L. Taylor, Mike R. Johnston
Publikováno v:
Geological Society, London, Special Publications. 442:41-54
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6612ffa610d211b8d2c5cea4a309b75a
https://doi.org/10.1144/sp442.17
https://doi.org/10.1144/sp442.17
Publikováno v:
Geological Society of America Bulletin. 104:429-443
The Dun Mountain ophiolite and overlying Maitai Group is discontinuously exposed for 480 km in South Island, New Zealand. Zircon U/Pb dates from plagiogranite are presented for relatively intact ophiolite, ophiolitic melanges, and for more silicic vo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a186dbd370bac8fa5054f0db15b210f8
https://doi.org/10.1130/0016-7606(1992)104<0429:ulaftd>2.3.co
https://doi.org/10.1130/0016-7606(1992)104<0429:ulaftd>2.3.co
Publikováno v:
New Zealand Journal of Geology and Geophysics. 29:291-301
In Croisilles Harbour area, sheared serpentinite and enclosed blocks of ophiolitic and sedimentary rock are interpreted as forming part of a tectonic unit, the Croisilles Melange. The melange separates poorly dated sedimentary rocks of the Rai Sandst
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::70c008d3a5b89c171de93732b0f26bd8
https://doi.org/10.1080/00288306.1986.10422152
https://doi.org/10.1080/00288306.1986.10422152