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1-20 OF 22 RESULTS FOR
Te Puke
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Journal Article
DIFFERENCES IN THE DEHYDRATION-REHYDRATION BEHAVIOR OF HALLOYSITES: NEW EVIDENCE AND INTERPRETATIONS Available to Purchase
Journal: Clays and Clay Minerals
Publisher: Clay Minerals Society
Published: 01 August 2006
Clays and Clay Minerals (2006) 54 (4): 473–484.
...Emmanuel Joussein; Sabine Petit; Claire-Isabelle Fialips; Philippe Vieillard; Dominique Righi Abstract Two reference halloysites from New Zealand (Te Puke and Opotiki) were studied by X-ray diffraction under (1) various levels of relative humidity (RH) from 95 to 0% (dehydration), and (2) various...
Image
XRD patterns of Ca-saturated Te Puke and Opotiki halloysite samples at vari... Available to Purchase
in DIFFERENCES IN THE DEHYDRATION-REHYDRATION BEHAVIOR OF HALLOYSITES: NEW EVIDENCE AND INTERPRETATIONS
> Clays and Clay Minerals
Published: 01 August 2006
Figure 2. XRD patterns of Ca-saturated Te Puke and Opotiki halloysite samples at various temperatures increasing from 25 (T 25 ) to 120°C (T 120 ).
Image
Effect of freeze-drying treatment on Opotiki and Te Puke samples Ca- or K-s... Available to Purchase
in DIFFERENCES IN THE DEHYDRATION-REHYDRATION BEHAVIOR OF HALLOYSITES: NEW EVIDENCE AND INTERPRETATIONS
> Clays and Clay Minerals
Published: 01 August 2006
Figure 5. Effect of freeze-drying treatment on Opotiki and Te Puke samples Ca- or K-saturated. K, K-FD, and Ca-FD mean K-saturated, K-saturated and freeze-dried, and Ca-saturated and freeze-dried, respectively. * refers to the 8.4 Å peak due to amphibole.
Image
XRD patterns of the Ca- and K-saturated Te Puke and Opotiki halloysite samp... Available to Purchase
in DIFFERENCES IN THE DEHYDRATION-REHYDRATION BEHAVIOR OF HALLOYSITES: NEW EVIDENCE AND INTERPRETATIONS
> Clays and Clay Minerals
Published: 01 August 2006
Figure 1. XRD patterns of the Ca- and K-saturated Te Puke and Opotiki halloysite samples recorded under various relative humidities (RH) decreasing from 95 to ~0% RH ( T = 27°C). * refers to the 8.4 Å peak due to amphibole.
Image
DTA-TGA curves for Te Puke and Opotiki samples (previously Ca saturated) at... Available to Purchase
in DIFFERENCES IN THE DEHYDRATION-REHYDRATION BEHAVIOR OF HALLOYSITES: NEW EVIDENCE AND INTERPRETATIONS
> Clays and Clay Minerals
Published: 01 August 2006
Figure 4. DTA-TGA curves for Te Puke and Opotiki samples (previously Ca saturated) at 40% and 0.2% RH. Dotted line represents the TGA.
Image
IR spectra (KBr pellets) of three New Zealand reference halloysites: (A) Op... Available to Purchase
Published: 01 December 2005
F ig . 7. IR spectra (KBr pellets) of three New Zealand reference halloysites: (A) Opotiki; (B) Matauri Bay; and (C) Te Puke.
Image
XRD powder patterns of three New Zealand references halloysites: (a) Opotik... Available to Purchase
Published: 01 December 2005
F ig . 5. XRD powder patterns of three New Zealand references halloysites: (a) Opotiki; (b) Te Puke, and (c) Matauri Bay. * and § refer to quartz and feldspars, respectively.
Image
TEM images of the three main morphologies of halloysite from New Zealand: (... Available to Purchase
Published: 01 December 2005
F ig . 2. TEM images of the three main morphologies of halloysite from New Zealand: (a) spheroidal (Opotiki); (b) short-tubes (Te Puke); and (c) large-tubes (Matauri Bay).
Image
Effect of ethylene glycol solvation before (lower) and after (upper) treatm... Available to Purchase
Published: 01 December 2005
F ig . 10. Effect of ethylene glycol solvation before (lower) and after (upper) treatment for three New Zealand references halloysites: (a) Opotiki; (b) Matauri Bay; and (c) Te Puke.
Image
XRD patterns of oriented preparation before (lower) and after (upper) forma... Available to Purchase
Published: 01 December 2005
F ig . 9. XRD patterns of oriented preparation before (lower) and after (upper) formamide treatment of three New Zealand references halloysites: (a) Opotiki, (b) Matauri Bay, and (c) Te Puke.
Image
XRD patterns obtained after dehydration from 95% RH to 0% RH, then rehydrat... Available to Purchase
in DIFFERENCES IN THE DEHYDRATION-REHYDRATION BEHAVIOR OF HALLOYSITES: NEW EVIDENCE AND INTERPRETATIONS
> Clays and Clay Minerals
Published: 01 August 2006
Figure 6. XRD patterns obtained after dehydration from 95% RH to 0% RH, then rehydration at 95% RH for Te Puke and Opotiki samples previously Ca- or K-saturated. * refers to the 8.4 Å peak due to amphibole.
Image
Computational fitting of the XRD profiles obtained for the Ca-saturated Te ... Available to Purchase
in DIFFERENCES IN THE DEHYDRATION-REHYDRATION BEHAVIOR OF HALLOYSITES: NEW EVIDENCE AND INTERPRETATIONS
> Clays and Clay Minerals
Published: 01 August 2006
Figure 3. Computational fitting of the XRD profiles obtained for the Ca-saturated Te Puke samples heat-treated at 30, 35, 40 and 50°C, and for the Ca-saturated Opotiki samples heat-treated at 40, 45, 55, 60 and 90°C.
Image
Effects of rehydration over a 3month period in liquid water after freeze-dr... Available to Purchase
in DIFFERENCES IN THE DEHYDRATION-REHYDRATION BEHAVIOR OF HALLOYSITES: NEW EVIDENCE AND INTERPRETATIONS
> Clays and Clay Minerals
Published: 01 August 2006
Figure 8. Effects of rehydration over a 3month period in liquid water after freeze-drying treatment of the K-saturated Opotiki and Te Puke halloysites. K, K-FD and K-FD-Ca-H 2 O mean K saturated, K saturated and freeze dried, and K saturated, freeze dried, Ca saturated and stored for 3 months
Image
Effects of rehydration over a 3 month period in liquid water after heat tre... Available to Purchase
in DIFFERENCES IN THE DEHYDRATION-REHYDRATION BEHAVIOR OF HALLOYSITES: NEW EVIDENCE AND INTERPRETATIONS
> Clays and Clay Minerals
Published: 01 August 2006
Figure 7. Effects of rehydration over a 3 month period in liquid water after heat treatment of the K-saturated Opotiki and Te Puke halloysites. K, K-100, and K-100-Ca-H 2 O mean K saturated, K saturated and heat treated at 100°C for one night, and K saturated, heat treated at 100°C, Ca saturated
Image
TEM images showing the shapes and sizes of some halloysite particles in rel... Available to Purchase
in Unique but diverse: some observations on the formation, structure and morphology of halloysite
> Clay Minerals
Published: 01 June 2016
Fig. 9. TEM images showing the shapes and sizes of some halloysite particles in relation to their Fe contents: (a) Te Puke (New Zealand), mostly platy, 0.2% Fe 2 O 3 as external oxides; (b) Matauri Bay (New Zealand), thick tubes, no external Fe oxide; (c) Jarrahdale (Australia), short tubes
Journal Article
Halloysite clay minerals — a review Available to Purchase
Journal: Clay Minerals
Published: 01 December 2005
Clay Minerals (2005) 40 (4): 383–426.
...F ig . 7. IR spectra (KBr pellets) of three New Zealand reference halloysites: (A) Opotiki; (B) Matauri Bay; and (C) Te Puke. ...
Journal Article
Unique but diverse: some observations on the formation, structure and morphology of halloysite Available to Purchase
Journal: Clay Minerals
Published: 01 June 2016
Clay Minerals (2016) 51 (3): 395–416.
...Fig. 9. TEM images showing the shapes and sizes of some halloysite particles in relation to their Fe contents: (a) Te Puke (New Zealand), mostly platy, 0.2% Fe 2 O 3 as external oxides; (b) Matauri Bay (New Zealand), thick tubes, no external Fe oxide; (c) Jarrahdale (Australia), short tubes...
Journal Article
Volcanic crustal structure of the western Hikurangi Plateau (New Zealand) from marine seismic reflection imaging Open Access
Andrew C. Gase, Nathan L. Bangs, Harm J.A. Van Avendonk, Dan Bassett, Stuart Henrys, Ryuta Arai, Gou Fujie, Philip M. Barnes, Shuichi Kodaira, Daniel H.N. Barker, David Okaya
Journal: Geosphere
Publisher: Geological Society of America
Published: 25 April 2024
Geosphere (2024) 20 (3): 935–964.
... CE is plotted in red (shallow; i.e., < 20 km) and blue (deep; i.e., >20 km) contours ( Wallace, 2020 ). From the upper horizon of Unit HKB, we interpret at least seven major seamounts along the margin, including Tūranganui Knoll, Puke Knoll, Te Kuri-a-Paoa Seamount, Māhia Seamount...
Journal Article
Epithermal Au-Ag and Related Deposits of the Hauraki Goldfield, Coromandel Volcanic Zone, New Zealand Available to Purchase
Journal: Economic Geology
Publisher: Society of Economic Geologists
Published: 01 August 2007
Economic Geology (2007) 102 (5): 785–816.
... in the Coromandel volcanic zone ( Skinner, 1986 ), North Island, New Zealand, contains about 50 epithermal Au-Ag deposits in a north-south–oriented belt, 200 km long by up to 40 km wide, extending from Great Barrier Island to Te Puke (Figs. 1 , 2 ; Table 1 ). The deposits are quartz ± calcite ± adularia ± illite...
Journal Article
Punctuated Evolution of a Large Epithermal Province: The Hauraki Goldfield, New Zealand Available to Purchase
Journal: Economic Geology
Publisher: Society of Economic Geologists
Published: 01 September 2011
Economic Geology (2011) 106 (6): 921–943.
... Report M183 . Rabone S.D.C. , 2006a , Broken Hills rhyolite-hosted high level epithermal vein system, Hauraki goldfield—100 years on : Australasian Institute of Mining and Metallurgy Monograph 25 , p. 117 – 122 . Rabone S.D.C. , 2006b , Exploration at Te Puke, Hauraki goldfield...
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