Temporal and spatial composition of water dissolved load in a temperate-glaciated catchment, the Waitaki Catchment, South Island, New Zealand.
The dissolved load of waters were analysed seasonally across a year (Summer - 2013 to Spring - 2014) using major and trace ions and Sr isotope ratios (87Sr/86Sr) to determine mineral provenance in the Waitaki Catchment, South Island, New Zealand. The Waitaki Catchment extends from the central-eastern section of the Southern Alps, through basin and range topography and finally through low-land farm land to the Pacific Ocean. It is New Zealand
xii, 201 pages A4
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MULTIPOLYGON (((171.120140577022 -44.994130324073,170.636607630983 -44.9166673553198,169.608596614219 -44.6555391892717,169.391467030384 -44.3898471425351,169.505134405591 -43.9437872786291,169.971655130165 -43.6831742408364,170.26709934323 -43.5923600353768,170.553387912081 -43.5035593201511,170.662437294922 -43.6457997557866,170.6310428557 -43.9220820860802,170.50519866964 -44.1724989800316,170.646654660454 -44.3601086079133,170.58818375897 -44.6715165054841,170.651156705399 -44.7651268098259,171.052176527562 -44.8947424055279,171.182049176107 -44.8939071066853,171.120140577022 -44.994130324073)))
Pettinger, Vincent (Vince), “Temporal and spatial composition of water dissolved load in a temperate-glaciated catchment, the Waitaki Catchment, South Island, New Zealand.,” Otago Geology Theses, accessed January 22, 2018, http://theses.otagogeology.org.nz/items/show/639.