D. Jerram, D. Jerram, John Millett, J. Kück, D. Thomas, S. Planke, E. Haskins, N. Lautze, S. Pierdominici
{"title":"了解地下火山相:夏威夷大岛PTA2和KMA1井的综合岩心、电缆测井和图像测井数据集","authors":"D. Jerram, D. Jerram, John Millett, J. Kück, D. Thomas, S. Planke, E. Haskins, N. Lautze, S. Pierdominici","doi":"10.5194/SD-25-15-2019","DOIUrl":null,"url":null,"abstract":"Abstract. To help understand volcanic facies in the subsurface, data sets\nthat enable detailed comparisons between down-hole geophysical data and cored\nvolcanic intervals are critical. However, in many cases, the collection of\nextended core intervals within volcanic sequences is rare and often\nincomplete due to challenging coring conditions. In this contribution we\noutline and provide initial results from borehole logging operations within\ntwo fully cored lava-dominated borehole sequences, PTA2 and KMA1, on the Big\nIsland of Hawai`i. Data for spectral gamma, magnetic susceptibility, dipmeter\nresistivity, sonic, total magnetic field, temperature and televiewer wireline\nlogs were successfully acquired for the open hole interval ca. 889 m to 1567 m within the PTA2 borehole. Spectral gamma was also collected from inside the\ncasing of both wells, extending the coverage for PTA2 to the surface and\ncovering the interval from ca. 300 to 1200 m for KMA1. High-quality core\nmaterial was available for both boreholes with almost complete recovery which\nenabled high-resolution core-to-log integration. Gamma data are generally low\ncommonly in the range ca. 7–20 gAPI but are shown to increase up to API of\nca. 60 with some intrusions and with increases in hawaiite compositions in\nthe upper part of PTA2. Velocity data are more variable due to alteration\nwithin porous volcanic facies than with burial depth, with a general degrease\ndown-hole. The high-resolution televiewer data have been compared directly to\nthe core, enabling a comprehensive analysis of the variations in the\nteleviewer responses. This has enabled the identification of key features\nincluding individual vesicles, vesicle segregations, strained vesicles,\nchilled margins, rubble zones, intrusive contacts and pāhoehoe lobe\nmorphologies, which can be confidently matched between the televiewer data\nand the full diameter core. The data set and results of this study include\nfindings which should enable improved borehole facies analysis through\nvolcanic sequences in the future, especially where down-borehole data and images\nbut no core are available.\n","PeriodicalId":51840,"journal":{"name":"Scientific Drilling","volume":"113 1","pages":""},"PeriodicalIF":1.6000,"publicationDate":"2019-06-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"20","resultStr":"{\"title\":\"Understanding volcanic facies in the subsurface: a combined core, wireline logging and image log data set from the PTA2 and KMA1 boreholes, Big Island, Hawai`i\",\"authors\":\"D. Jerram, D. Jerram, John Millett, J. Kück, D. Thomas, S. Planke, E. Haskins, N. Lautze, S. Pierdominici\",\"doi\":\"10.5194/SD-25-15-2019\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Abstract. To help understand volcanic facies in the subsurface, data sets\\nthat enable detailed comparisons between down-hole geophysical data and cored\\nvolcanic intervals are critical. However, in many cases, the collection of\\nextended core intervals within volcanic sequences is rare and often\\nincomplete due to challenging coring conditions. In this contribution we\\noutline and provide initial results from borehole logging operations within\\ntwo fully cored lava-dominated borehole sequences, PTA2 and KMA1, on the Big\\nIsland of Hawai`i. Data for spectral gamma, magnetic susceptibility, dipmeter\\nresistivity, sonic, total magnetic field, temperature and televiewer wireline\\nlogs were successfully acquired for the open hole interval ca. 889 m to 1567 m within the PTA2 borehole. Spectral gamma was also collected from inside the\\ncasing of both wells, extending the coverage for PTA2 to the surface and\\ncovering the interval from ca. 300 to 1200 m for KMA1. High-quality core\\nmaterial was available for both boreholes with almost complete recovery which\\nenabled high-resolution core-to-log integration. Gamma data are generally low\\ncommonly in the range ca. 7–20 gAPI but are shown to increase up to API of\\nca. 60 with some intrusions and with increases in hawaiite compositions in\\nthe upper part of PTA2. Velocity data are more variable due to alteration\\nwithin porous volcanic facies than with burial depth, with a general degrease\\ndown-hole. The high-resolution televiewer data have been compared directly to\\nthe core, enabling a comprehensive analysis of the variations in the\\nteleviewer responses. This has enabled the identification of key features\\nincluding individual vesicles, vesicle segregations, strained vesicles,\\nchilled margins, rubble zones, intrusive contacts and pāhoehoe lobe\\nmorphologies, which can be confidently matched between the televiewer data\\nand the full diameter core. The data set and results of this study include\\nfindings which should enable improved borehole facies analysis through\\nvolcanic sequences in the future, especially where down-borehole data and images\\nbut no core are available.\\n\",\"PeriodicalId\":51840,\"journal\":{\"name\":\"Scientific Drilling\",\"volume\":\"113 1\",\"pages\":\"\"},\"PeriodicalIF\":1.6000,\"publicationDate\":\"2019-06-12\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"20\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Scientific Drilling\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.5194/SD-25-15-2019\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Scientific Drilling","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5194/SD-25-15-2019","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
Understanding volcanic facies in the subsurface: a combined core, wireline logging and image log data set from the PTA2 and KMA1 boreholes, Big Island, Hawai`i
Abstract. To help understand volcanic facies in the subsurface, data sets
that enable detailed comparisons between down-hole geophysical data and cored
volcanic intervals are critical. However, in many cases, the collection of
extended core intervals within volcanic sequences is rare and often
incomplete due to challenging coring conditions. In this contribution we
outline and provide initial results from borehole logging operations within
two fully cored lava-dominated borehole sequences, PTA2 and KMA1, on the Big
Island of Hawai`i. Data for spectral gamma, magnetic susceptibility, dipmeter
resistivity, sonic, total magnetic field, temperature and televiewer wireline
logs were successfully acquired for the open hole interval ca. 889 m to 1567 m within the PTA2 borehole. Spectral gamma was also collected from inside the
casing of both wells, extending the coverage for PTA2 to the surface and
covering the interval from ca. 300 to 1200 m for KMA1. High-quality core
material was available for both boreholes with almost complete recovery which
enabled high-resolution core-to-log integration. Gamma data are generally low
commonly in the range ca. 7–20 gAPI but are shown to increase up to API of
ca. 60 with some intrusions and with increases in hawaiite compositions in
the upper part of PTA2. Velocity data are more variable due to alteration
within porous volcanic facies than with burial depth, with a general degrease
down-hole. The high-resolution televiewer data have been compared directly to
the core, enabling a comprehensive analysis of the variations in the
televiewer responses. This has enabled the identification of key features
including individual vesicles, vesicle segregations, strained vesicles,
chilled margins, rubble zones, intrusive contacts and pāhoehoe lobe
morphologies, which can be confidently matched between the televiewer data
and the full diameter core. The data set and results of this study include
findings which should enable improved borehole facies analysis through
volcanic sequences in the future, especially where down-borehole data and images
but no core are available.