title: Andesite volcanic facies and hydrothermal alteration in the subsurface peripheral to existing Waihi mine workings

authors: Bodger, Billy

subjects: Waihi

abstract: The Waihi vein system is an andesite-hosted epithermal Au-Ag deposit comprising a series of veins located in the southern Hauraki Goldfield, New Zealand. It includes the Martha Mine which is the largest gold producer in the Hauraki Goldfield. Despite a history of over 127 years of prospecting and mining at Waihi, the Favona Au-Ag deposit was recently discovered in blind quartz veins 2 km to the east of Martha Mine. This highlights that there are still new Au-Ag veins to be found and extensions of existing veins to be explored. Little work has been published on the volcanism of the Waipupu Formation andesites, which host the mineralisation. Secondly, the formation of epithermal mineral deposits is accompanied by various chemical reactions which occur between mineralising fluids and host rock, and commonly produce distinct mineralogical and geochemical halos that overprint the volcanic textures and are generally much larger than the ore bodies themselves. The overall aim of this project is, therefore, to reconstruct the volcanic and hydrothermal setting peripheral to the Martha Hill mine. Two northwest-oriented exploration drill holes that are peripheral to the Martha Hill vein system were logged from a volcanological perspective, sampled and analysed by optical mineralogy, TerraSpec, x-ray diffraction on clay separates and x-ray-fluorescence.

Eight new andesite lava facies have been recognised. Six of the facies were identified based on mineral abundances and the presence of quartz phenocrysts. The crystal abundances within these lava facies ranges from 10 to 60% and are dominated by feldspar and mafic minerals. Quartz phenocrysts are minor but prominent features in the rock. These mineral abundances are near synonymous with other active andesite volcanoes and Late Archean examples. The texture of each of the lava facies is dominantly porphyritic, and phenocrysts are mainly plagioclase + ferromagnesian silicates ± quartz. Quartz phenocrysts are commonly resorbed which reflects different levels of magma mixing within the magma chamber before erupting. The other two facies were andesite lava breccias described as either monolithic (containing one clast type) or heterolithic (containing multiple clast types). The monolithic breccia resembles that of an autobreccia, typically associated with the outer parts of a lava flow.

Using alteration mineralogy data (from shortwave infrared spectroscopy and x-ray diffraction on clay separates) and geochemical data (from x-ray fluorescence), a transition from illite to interstratified illite-smectite to smectite was identified heading northwest from the Martha Mine and major mineralised Au-Ag quartz veins. Based on known thermal stabilities for these minerals, a paleoisotherm model was established peripheral to the Martha Hill mine suggesting a “cooling” of the hydrothermal fluid northwest of Martha Mine. Multiple trace elements such as Tl, Bi and Se strongly correlated to the mineralogy, vectoring towards higher temperature mineralisation.

text: Andesite volcanic facies and hydrothermal alteration in the subsurface peripheral to existing Waihi mine workings The Waihi vein system is an andesite-hosted epithermal Au-Ag deposit comprising a series of veins located in the southern Hauraki Goldfield, New Zealand. It includes the Martha Mine which is the largest gold producer in the Hauraki Goldfield. Despite a history of over 127 years of prospecting and mining at Waihi, the Favona Au-Ag deposit was recently discovered in blind quartz veins 2 km to the east of Martha Mine. This highlights that there are still new Au-Ag veins to be found and extensions of existing veins to be explored. Little work has been published on the volcanism of the Waipupu Formation andesites, which host the mineralisation. Secondly, the formation of epithermal mineral deposits is accompanied by various chemical reactions which occur between mineralising fluids and host rock, and commonly produce distinct mineralogical and geochemical halos that overprint the volcanic textures and are generally much larger than the ore bodies themselves. The overall aim of this project is, therefore, to reconstruct the volcanic and hydrothermal setting peripheral to the Martha Hill mine. Two northwest-oriented exploration drill holes that are peripheral to the Martha Hill vein system were logged from a volcanological perspective, sampled and analysed by optical mineralogy, TerraSpec, x-ray diffraction on clay separates and x-ray-fluorescence.

Eight new andesite lava facies have been recognised. Six of the facies were identified based on mineral abundances and the presence of quartz phenocrysts. The crystal abundances within these lava facies ranges from 10 to 60% and are dominated by feldspar and mafic minerals. Quartz phenocrysts are minor but prominent features in the rock. These mineral abundances are near synonymous with other active andesite volcanoes and Late Archean examples. The texture of each of the lava facies is dominantly porphyritic, and phenocrysts are mainly plagioclase + ferromagnesian silicates ± quartz. Quartz phenocrysts are commonly resorbed which reflects different levels of magma mixing within the magma chamber before erupting. The other two facies were andesite lava breccias described as either monolithic (containing one clast type) or heterolithic (containing multiple clast types). The monolithic breccia resembles that of an autobreccia, typically associated with the outer parts of a lava flow.

Using alteration mineralogy data (from shortwave infrared spectroscopy and x-ray diffraction on clay separates) and geochemical data (from x-ray fluorescence), a transition from illite to interstratified illite-smectite to smectite was identified heading northwest from the Martha Mine and major mineralised Au-Ag quartz veins. Based on known thermal stabilities for these minerals, a paleoisotherm model was established peripheral to the Martha Hill mine suggesting a “cooling” of the hydrothermal fluid northwest of Martha Mine. Multiple trace elements such as Tl, Bi and Se strongly correlated to the mineralogy, vectoring towards higher temperature mineralisation.

year: 2015

title: Spatial Hypermedia as a programming environment

authors: Nemhauser, Bryce

subjects: Spatial Hypermedia

abstract: This thesis investigates the possibilities opened to a programmer when their programming environment not only utilises Spatial Hypermedia functionality, but embraces it as a core component. Designed and built to explore these possibilities, SpIDER (standing for Spatial Integrated Development Environment Research) is an IDE featuring not only traditional functionality such as content assist and debugging support but also multimedia integration and free-form spatial code layout. Such functionality allows programmers to visually communicate aspects of the intent and structure of their code that would be tedious—and in some cases impossible—to achieve in conventional IDEs.
Drawing from literature on Spatial Memory, the design of SpIDER has been driven by the desire to improve the programming experience while also providing a flexible authoring environment for software development. The programmer’s use of Spatial Memory is promoted, in particular, by: utilising fixed sized authoring canvases; providing the capacity for landmarks; exploiting a hierarchical linking system; and having well defined occlusion and spatial stability of authored code.
The key challenge in implementing SpIDER was to devise an algorithm to bridge the gap between spatially expressed source code, and the serial text forms required by compilers. This challenge was met by developing an algorithm that we have called the flow walker. We validated this algorithm through user testing to establish that participants’ interpretation of the meaning of spatially laid out code matched the flow walker’s implementation.
SpIDER can be obtained at: https://sourceforge.net/projects/spatial-ide-research-spider

text: Spatial Hypermedia as a programming environment This thesis investigates the possibilities opened to a programmer when their programming environment not only utilises Spatial Hypermedia functionality, but embraces it as a core component. Designed and built to explore these possibilities, SpIDER (standing for Spatial Integrated Development Environment Research) is an IDE featuring not only traditional functionality such as content assist and debugging support but also multimedia integration and free-form spatial code layout. Such functionality allows programmers to visually communicate aspects of the intent and structure of their code that would be tedious—and in some cases impossible—to achieve in conventional IDEs.
Drawing from literature on Spatial Memory, the design of SpIDER has been driven by the desire to improve the programming experience while also providing a flexible authoring environment for software development. The programmer’s use of Spatial Memory is promoted, in particular, by: utilising fixed sized authoring canvases; providing the capacity for landmarks; exploiting a hierarchical linking system; and having well defined occlusion and spatial stability of authored code.
The key challenge in implementing SpIDER was to devise an algorithm to bridge the gap between spatially expressed source code, and the serial text forms required by compilers. This challenge was met by developing an algorithm that we have called the flow walker. We validated this algorithm through user testing to establish that participants’ interpretation of the meaning of spatially laid out code matched the flow walker’s implementation.
SpIDER can be obtained at: https://sourceforge.net/projects/spatial-ide-research-spider

year: 2018

title: Kapa Haka Whakataetae Kua tini haere te kanohi o te mahi kapa haka i te ao hurihuri nei.

authors: Rollo, Te Manaaroha Pirihira

subjects: Kapa Haka

abstract: Tihei Haka! Mauriora Kapa haka (Rollo, 2006)
Ka tū te ihiihi, ka tū te wanawana o te hunga i ngā hui whakataetae kapa haka o te motu. He hui rongonui i te maramataka a te Māori ia tau ia tau, ā, he hui whakahirahira anō mō rātou mā i whakawhiti mai i tāwahi rā hoki. Mā te mahi a te kapa haka ka whakaari ngā rōpū haka i ngā mahi nō nehe rā me ngā mahi hou o te ao onāianei. Ahakoa te āhuatanga o te mahi, he taonga tuku iho nā rātou mā kua mene ki te pō.  Moe mai rā e te kāhui o ngā whetu i te pō, moe mai i te Ariki o te rangi. 

I tēnei tuhinga, e āta titiro ana 'hau ki ngā mahi hou me te āhuatanga hou kei ngā rōpū haka i te whakataetae-a-motu, arā Te Matatini me ētahi atu momo whakataetae i Aotearoa, tāpiri mai hoki ērā kei Te Moana nui a Kiwa. Ko te ingoa matua o tēnei tuhinga,  KAPA HAKA WHAKATAETAE. Kua tīni haere te kanohi o te mahi kapa haka i te ao hurihuri nei .
No reira, ko te tino pātai kei tēnei rangahau ko tērā. He aha ngā mahi hou kei te kapa haka whakataetae? Nā he hua anō hoki kei reira? Ka hāngaia tonu e te tuhinga nei  ngā hui whakataetae kapa haka mai i te tau 1972 tae noa ki te tau 2006.

Ngā ūpoko o te tuhinga whakapae
E whā ngā wāhanga ūpoko o tēnei tuhinga whakapae. Mā ngā ūpoko katoa ka kitea ai ngā momo kaupapa ake e hāngai pū ana ki te kaupapa mō te whakataetae kapa haka me ōna āhuatanga hou. He mahi whakahirahira tāku ki te whakatakoto i ngā kōrero, i ngā whakaaro, i ngā mātauranga o tēnā tangata mōhio, o tēnā tangata mātau ki roto i ngā whare māramatanga, arā ngā  wāhanga wēnā,  hei mātauranga hou mō te ao katoa.

I te ūpoko tuatahi, ka anga te titiro ki ngā whakamāramatanga o ngā tikanga-a-iwi e pā ana ki te  tūturutanga me te ao o te kapa haka. Mā wēnei whakamāramatanga hei awhi i a 'hau i taku rangahau ki te mahi onāianei o te whakataetae kapa haka. Ka whai mātauranga 'hau mō ngā tikanga o ngā kupu e rua. Ko ēnei ko te kupu  haka  te tuatahi, ā, ko te kupu  kapa haka  te tuarua. He aha ngā rerekētanga me te ōritenga o wēnei kupu rongonui? Ka anga whakamua ki ngā tūmanako me ngā ritenga o te whakataetae kapa haka a te motu mai i te New Zealand Polynesian Festival tae atu ki Te Matatini. Ko te whāinga mutunga o tēnei wāhanga, ka hoki whakanui ki te whakataetae-a-motu mai i te tau 1972 tae noa atu ki te tau 2006.

Ko te ūpoko tuarua, ka whakatakoto e 'hau ngā whakautu o ngā patapātai mai i ngā rārangi kōrero me ngā whakaaro whānui i whakahokia mai e ngā tāngata o ngā rōpū haka e whā, arā, Te Rōpū Haka o Te Kotahitanga, Ngāti Poneke Young Māori Club, ko Te Waihīrere, ā, huri atu ki Te Pou a Mangatāwhiri hoki, he rōpū i whakatūhia anō i te tau 2005. I tēnei wāhanga ka kitea ngā kōrero ātaahua, ngā mātauranga tūturu me ngā whakaaro hōhonu o ngā kaiako me ngā tāngata e tautoko ana i taku mahi kimi mātauranga.  Nā rātou ka ohorere, ka mirimiri hoki i tōku hinengaro ki ngā māramatanga hou. He tika anō te kupu ā  Pā Henare Tate nō Ngapuhi nui tonu e kī ana,  Mā te whakaatu, ka mōhio, mā te mōhio, ka mārama, mā te mārama, ka mātau, mā te mātau, ka ora   (Barlow 1991)

I te ūpoko tuatoru he whakaaturanga tēnei o āku tirohanga ki ngā āhua rerekē me ngā mahi hou i roto i ngā rōpū haka i runga i te ātamira o te whakataetae, i roto hoki i te mura o te ahi o te whakataetae. Kua tuhituhi au i ngā momo āhuatanga e pā ana ki  te taha o te kanikani, te mahi-a-korikori me ngā mahi katoa i runga i te atamira. Ahakoa iti ko tētahi atu wahanga o ērā kōrero e pā ana ki te pūoro me ōna mana kua puta i konei. Ka huri taku tuhinga ki te taha o te reo waiata, te toi whakaari me te whakaataata o ngā mahi a te Rēhia. I konei ka titiro ki te tāmoko, te pani kanohi me te pani tinana, arā he mahi hou katoa. Ko te wahanga mutunga e pā ana ki te reo Māori me te tito waiata hoki. Ahakoa he maha ngā āhuatanga, ko ngā tuhinga nei mō ia āhuatanga kia kitea ai ngā rerekēnga me ngā mahi hou i te whakataetae kapa haka o te ao Māori. No reira te nuinga engari ko wētahi i whakaurua mai i ētahi atu iwi ō tāwahi.       

Ko te ūpoko whakamutunga, ka hāngai taku titiro ki te ao o te whakataetae, arā, ki ngā whakaaro me te tā o te hinengaro me te ngākau o te tangata. Ka peka haere ki te whakatū o ngā rōpū whakataetae me te parakatihi o ngā waiata, ngā haka me ngā whakaritenga mo te whakataetae kapa haka. Ko te kōrero whakamutunga, ka huri ki wētahi atu o ngā whakataetae mai i Te Kuki Airani, i Tahiti me Hawaii hoki. Āe mārika, ka ora te ao o te whakataetae puta noa i te ao nui. Ki ahau, mā tēnei tuhinga hei whakapuare ngā hurihanga o te ao Māori me te ao o te kapa haka. Ka ea, he tika hoki te whakataukī rā,  ka pū te ruha, ka hao te rangatahi    (Ryan 1995), arā ka kimi i ērā e pīataata ai o rātou wairua, hinengaro, ngākau.

text: Kapa Haka Whakataetae Kua tini haere te kanohi o te mahi kapa haka i te ao hurihuri nei. Tihei Haka! Mauriora Kapa haka (Rollo, 2006)
Ka tū te ihiihi, ka tū te wanawana o te hunga i ngā hui whakataetae kapa haka o te motu. He hui rongonui i te maramataka a te Māori ia tau ia tau, ā, he hui whakahirahira anō mō rātou mā i whakawhiti mai i tāwahi rā hoki. Mā te mahi a te kapa haka ka whakaari ngā rōpū haka i ngā mahi nō nehe rā me ngā mahi hou o te ao onāianei. Ahakoa te āhuatanga o te mahi, he taonga tuku iho nā rātou mā kua mene ki te pō.  Moe mai rā e te kāhui o ngā whetu i te pō, moe mai i te Ariki o te rangi. 

I tēnei tuhinga, e āta titiro ana 'hau ki ngā mahi hou me te āhuatanga hou kei ngā rōpū haka i te whakataetae-a-motu, arā Te Matatini me ētahi atu momo whakataetae i Aotearoa, tāpiri mai hoki ērā kei Te Moana nui a Kiwa. Ko te ingoa matua o tēnei tuhinga,  KAPA HAKA WHAKATAETAE. Kua tīni haere te kanohi o te mahi kapa haka i te ao hurihuri nei .
No reira, ko te tino pātai kei tēnei rangahau ko tērā. He aha ngā mahi hou kei te kapa haka whakataetae? Nā he hua anō hoki kei reira? Ka hāngaia tonu e te tuhinga nei  ngā hui whakataetae kapa haka mai i te tau 1972 tae noa ki te tau 2006.

Ngā ūpoko o te tuhinga whakapae
E whā ngā wāhanga ūpoko o tēnei tuhinga whakapae. Mā ngā ūpoko katoa ka kitea ai ngā momo kaupapa ake e hāngai pū ana ki te kaupapa mō te whakataetae kapa haka me ōna āhuatanga hou. He mahi whakahirahira tāku ki te whakatakoto i ngā kōrero, i ngā whakaaro, i ngā mātauranga o tēnā tangata mōhio, o tēnā tangata mātau ki roto i ngā whare māramatanga, arā ngā  wāhanga wēnā,  hei mātauranga hou mō te ao katoa.

I te ūpoko tuatahi, ka anga te titiro ki ngā whakamāramatanga o ngā tikanga-a-iwi e pā ana ki te  tūturutanga me te ao o te kapa haka. Mā wēnei whakamāramatanga hei awhi i a 'hau i taku rangahau ki te mahi onāianei o te whakataetae kapa haka. Ka whai mātauranga 'hau mō ngā tikanga o ngā kupu e rua. Ko ēnei ko te kupu  haka  te tuatahi, ā, ko te kupu  kapa haka  te tuarua. He aha ngā rerekētanga me te ōritenga o wēnei kupu rongonui? Ka anga whakamua ki ngā tūmanako me ngā ritenga o te whakataetae kapa haka a te motu mai i te New Zealand Polynesian Festival tae atu ki Te Matatini. Ko te whāinga mutunga o tēnei wāhanga, ka hoki whakanui ki te whakataetae-a-motu mai i te tau 1972 tae noa atu ki te tau 2006.

Ko te ūpoko tuarua, ka whakatakoto e 'hau ngā whakautu o ngā patapātai mai i ngā rārangi kōrero me ngā whakaaro whānui i whakahokia mai e ngā tāngata o ngā rōpū haka e whā, arā, Te Rōpū Haka o Te Kotahitanga, Ngāti Poneke Young Māori Club, ko Te Waihīrere, ā, huri atu ki Te Pou a Mangatāwhiri hoki, he rōpū i whakatūhia anō i te tau 2005. I tēnei wāhanga ka kitea ngā kōrero ātaahua, ngā mātauranga tūturu me ngā whakaaro hōhonu o ngā kaiako me ngā tāngata e tautoko ana i taku mahi kimi mātauranga.  Nā rātou ka ohorere, ka mirimiri hoki i tōku hinengaro ki ngā māramatanga hou. He tika anō te kupu ā  Pā Henare Tate nō Ngapuhi nui tonu e kī ana,  Mā te whakaatu, ka mōhio, mā te mōhio, ka mārama, mā te mārama, ka mātau, mā te mātau, ka ora   (Barlow 1991)

I te ūpoko tuatoru he whakaaturanga tēnei o āku tirohanga ki ngā āhua rerekē me ngā mahi hou i roto i ngā rōpū haka i runga i te ātamira o te whakataetae, i roto hoki i te mura o te ahi o te whakataetae. Kua tuhituhi au i ngā momo āhuatanga e pā ana ki  te taha o te kanikani, te mahi-a-korikori me ngā mahi katoa i runga i te atamira. Ahakoa iti ko tētahi atu wahanga o ērā kōrero e pā ana ki te pūoro me ōna mana kua puta i konei. Ka huri taku tuhinga ki te taha o te reo waiata, te toi whakaari me te whakaataata o ngā mahi a te Rēhia. I konei ka titiro ki te tāmoko, te pani kanohi me te pani tinana, arā he mahi hou katoa. Ko te wahanga mutunga e pā ana ki te reo Māori me te tito waiata hoki. Ahakoa he maha ngā āhuatanga, ko ngā tuhinga nei mō ia āhuatanga kia kitea ai ngā rerekēnga me ngā mahi hou i te whakataetae kapa haka o te ao Māori. No reira te nuinga engari ko wētahi i whakaurua mai i ētahi atu iwi ō tāwahi.       

Ko te ūpoko whakamutunga, ka hāngai taku titiro ki te ao o te whakataetae, arā, ki ngā whakaaro me te tā o te hinengaro me te ngākau o te tangata. Ka peka haere ki te whakatū o ngā rōpū whakataetae me te parakatihi o ngā waiata, ngā haka me ngā whakaritenga mo te whakataetae kapa haka. Ko te kōrero whakamutunga, ka huri ki wētahi atu o ngā whakataetae mai i Te Kuki Airani, i Tahiti me Hawaii hoki. Āe mārika, ka ora te ao o te whakataetae puta noa i te ao nui. Ki ahau, mā tēnei tuhinga hei whakapuare ngā hurihanga o te ao Māori me te ao o te kapa haka. Ka ea, he tika hoki te whakataukī rā,  ka pū te ruha, ka hao te rangatahi    (Ryan 1995), arā ka kimi i ērā e pīataata ai o rātou wairua, hinengaro, ngākau.

year: 2007