✦ LIBER ✦

95/01622 Geochemical structure and position of the Waiotapu geothermal field, New Zealand

Publisher: Elsevier Science
Year: 1995
Weight: 213 KB
Volume: 36
Category: Article
ISSN: 0140-6701
DOI: 10.1016/0140-6701(95)93287-9

No coin nor oath required. For personal study only.

📜 SIMILAR VOLUMES

95/01626 Resistivity structure of the Wa

95/01626 Resistivity structure of the Waimangu, Waiotapu, Waikite and Reporoa Geothermal areas, New Zealand

📂 Article 📅 1995 🏛 Elsevier Science ⚖ 213 KB

95/01627 Stratigraphy, paleomagnetism, g

95/01627 Stratigraphy, paleomagnetism, geochronology and structure of silicic volcanic rocks, Waiotapu/Paeroa range area, New Zealand

📂 Article 📅 1995 🏛 Elsevier Science ⚖ 213 KB

Appraisal of the Tokaanu–Waihi geotherma

Appraisal of the Tokaanu–Waihi geothermal field and its relationship with the Tongariro geothermal field, New Zealand

✍ George F Risk; Hugh M Bibby; Christopher J Bromley; T.Grant Caldwell; Stewart L 📂 Article 📅 2002 🏛 Elsevier Science 🌐 English ⚖ 929 KB

Tokaanu-Waihi geothermal field is situated near the southern end of the Taupo Volcanic Zone, New Zealand. Neutral chloride thermal waters discharge at Tokaanu and Waihi in the north of the field on flat land between the andesite volcanoes Tihia and Kakaramea and the shore of Lake Taupo, while steam-

Resistivity structure of the Waimangu Wa

Resistivity structure of the Waimangu Waiotapu, Waikite and Reporoa geothermal areas, New Zealand : H. M. Bibby, S. L. Bennie, V. M. Stagpoole & T. G. Caldwell, Geothermics, 23(5–6), 1994, pp 445–471

📂 Article 📅 1995 🏛 Elsevier Science 🌐 English ⚖ 134 KB

Chemical and isotopic changes in shallow

Chemical and isotopic changes in shallow groundwater caused by exploitation of the Wairakei geothermal field, New Zealand

✍ Richard B. Glover; Michael K. Stewart 📂 Article 📅 1996 🏛 Elsevier Science 🌐 English ⚖ 850 KB

Chemical data obtained in 1983/84 and 1994 from groundwater monitor wells at Wairakei are reviewed and interpreted in conjunction with physical changes in the deeper system. The composition of the waters is controlled by the proportion of deep chloride, shallow meteoric and steamheated components. T