石油技術協会誌
Online ISSN : 1881-4131
Print ISSN : 0370-9868
ISSN-L : 0370-9868
83 巻, 4 号
石油技術協会誌
選択された号の論文の5件中1~5を表示しています
講演
  • 露頭からベースンへ
    栗田 裕司
    原稿種別: 講演
    2018 年 83 巻 4 号 p. 239-245
    発行日: 2018/10/22
    公開日: 2021/01/09
    ジャーナル フリー

    The geology of the northern Niigata area, northern Honshu, Japan, provides a template of the petroleum system including Miocene source rock and Pliocene -Pleistocene turbidite sandstone reservoirs that resulted in number of commercial fields in this particular area. In contrast, the Yamagata area to the north of northern Niigata is characterized by uplifted and dissected blocks of basement rocks and Miocene sedimentary covers, which permits easier access to lateral changes of Miocene lithofacies. Recent investigation on biosiliceous shale in these areas seems to be raising new ideas on source rock generation in the Miocene back-arc setting. Our intention includes tight reservoir exploration, a growing concept in this country, in the Miocene biosiliceous shale formations like in the Monterey Formation of the US Pacific coast. As pursuit of new ideas like this has to be inherited by young generation of petroleum geologists/engineers, promoting collaborative activities between the industries and educational sectors should be the most helpful foothold for our future to come.

  • 和久津 英志
    原稿種別: 講演
    2018 年 83 巻 4 号 p. 246-250
    発行日: 2018/10/22
    公開日: 2021/01/09
    ジャーナル フリー
  • 廣野 耕造
    原稿種別: 講演
    2018 年 83 巻 4 号 p. 251-256
    発行日: 2018/10/22
    公開日: 2021/01/09
    ジャーナル フリー

    On January 1st, 2019, The city of Niigata marks the 150th anniversary of the opening of Niigata port.

    Throughout the history of Niigata, Niigata port has a crucial role to create the unique history and culture. In prehistoric time, Niigata port presumed already existed, even if water traffic was primitive era. “Kanbara-no-tsu” is the first set up port described at Engi-Shiki in 972 A.D. Then, “Nuttari-minato” port and “Niigata-no-tsu” port appeared from the 14th to the 16th century. As described three ports were located at the mouths of the Shinano river and the Agano river, these two rivers have the largest watershed area in Japan. In early modern ages, Niigata port became prosperous as a port of Kitamaebune cargo ships entrance and departure. In the period of Isolation, the end of the Edo era,foreign countries selected led to be forced to opening of Niigata port, however, due to the civil war, it opened later than the other ports.

    After the Meiji era, Niigata thrived as a modern port and also as a gateway to the continent, but towards the end of WWII, the port lost all ability to function due to a naval mine blockade in the surrounding waters. After the war, the port regained its position as one of the Japanese most important ports. Today, many cultural assets from Port City Niigataʼs history remain including the traditional Ryoutei restaurants and Geisha culture that blossomed to welcome guests when Niigata flourished as a trading hub, former residences of wealthy merchants from that same period, and cultural assets related to praying for ship safety. Port City Niigata will continue to utilize these cultural legacies to better our city.

報告
  • 加藤 進
    原稿種別: 報告
    2018 年 83 巻 4 号 p. 257-266
    発行日: 2018/10/22
    公開日: 2021/01/09
    ジャーナル フリー

    Chemical and isotopic compositions of formation waters from oil and gas fields in Niigata Prefecture, Japan, were examined to demonstrate their geochemical characteristics and stratigraphic change for each formation.

    They have the following geochemical characteristics.

    1) The formation waters are mainly composed of Na and Cl ions.

    2) Although they were originated from seawater (Kato and Kajiwara, 1986), their SO42- and Mg2+ contents have decreased rapidly and their NH4, I and HCO3 contents which are derived from organic matter have

    increased roughly in this order during burial diagenesis.

    3) They have a relative narrow range of δD values between -15 and -3 ‰ and large variations of δ18O values from -4.8 to +1.6 ‰, similar to formation waters from oil and gas fields in Akita, Japan.

    Their Cl contents reach the maximum in the upper part of the Nishiyama Formation which is due to formation of authigenic minerals such as clay mineral and zeolite from volcanic glass, and decrease toward the underlying Shiiya and Teradomari formations. This decrease of Cl content may be caused by release of waters from transformation of clay minerals and maturation of organic matter during burial of sediments.

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