[1]王照波,王江月,張 劍.山東蒙山第四紀冰川、黃土、水系沉積物與MIS對比研究[J].華東地質,2019,40(02):81.
 WANG Zhao-bo,WANG Jiang-yue,ZHANG Jian.Comparison Quaternary Sediments of Glaciers, Loess, Stream with Marine Isotope Stages(MIS) in Mengshan, Shandong[J].East China Geology,2019,40(02):81.
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山東蒙山第四紀冰川、黃土、水系沉積物與MIS對比研究()
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《華東地質》[ISSN:2096-1871/CN:32-1865/P]

卷:
40
期數:
2019年02期
頁碼:
81
欄目:
基礎地質
出版日期:
2019-06-01

文章信息/Info

Title:
Comparison Quaternary Sediments of Glaciers, Loess, Stream with Marine Isotope Stages(MIS) in Mengshan, Shandong
作者:
王照波123王江月4張 劍 5
(1.山東指南針礦產勘查有限公司,臨沂 276006; 2.沂蒙山國家地質公園管理局,臨沂 273304; 3.國土資源部金礦成礦過程與資源利用重點實驗室,濟南 250013; 4. 曲阜師范大學 地理與旅游學院,日照 276800; 5. 青島海洋地質研究所,青島 266071)
Author(s):
WANG Zhao-bo123WANG Jiang-yue4ZHANG Jian5
(1. Shandong Compass Mineral Exploration co., Ltd , Linyi 276006,China;2. Yimeng national geological park management office, Linyi 273304,China;3.Laboratory of Gold Mineralization Process and Resource Utilization, Ministry of Natural Resources, Jinan 250013,China; 4. College of geography and travel, Qufu Normal University, Qufu 276800,China;5.Qingdao Institute of marine geology, China Geological Survey, Qingdao 266071,China)
關鍵詞:
冰川遺跡黃土MIS第四紀蒙山山東
Keywords:
Glacier Relics Loess Marine Isotope Stages(MIS) Quaternary Mengshan Shandong
文獻標志碼:
A
摘要:
為了確定山東蒙山佛塔谷一帶的第四紀冰川、黃土、水系沉積物與MIS的對應關系,對該區冰川遺跡進行了詳細調查,并對冰川、黃土和水系沉積物進行年代學研究。對比研究了蒙山地區各類地層沉積與深海氧同位素演化階段的對應性,建立了冰川、黃土、水系沉積物與環境演化的內在關系;詳細對比了全新世、晚更新世冰川、黃土、水系沉積物與MIS的關系,初步對比了中更新世冰川沉積物與MIS的關系,發現我國東部各類第四紀沉積物與MIS之間具有良好的對應關系,從沉積層序與環境演化的角度,確認了蒙山及我國東部地區存在第四紀冰川作用的事實。
Abstract:
The study conducted the research on glacier relics and the sediments of glaciers, loess, stream using geochronology, which confirmed the corresponding relationship between the sediments of quaternary glacier, loess, stream and Marine Isotope Stages (MIS) in Pagoda Valley of Mengshan. And on this basis, it was the first time to study the relativity between all kinds of stratum sediments and Marine Isotope Stages(MIS) in Mengshan, and the intrinsic relationship between the sediments of glacier, loess, stream and environmental evolution was established. Comparing these sediments and Marine Isotope Stages(MIS) especially in Holocene and late Pleistocene found that it is a strong relationship between these Quaternary sediments and Marine Isotope Stages(MIS) and confirmed the fact that the existence of Quaternary glacial through the sedimentary sequence and environment evolution in Mengshan and eastern China.

備注/Memo

備注/Memo:
收稿日期:2018-05-14 修訂日期:2018-08-10 責任編輯:譚桂麗
基金項目:國土資源部金礦成礦過程與資源利用重點實驗室 “山東金剛石成礦規律與侵位時代研究(編號:201403)”和山東指南針礦產勘查有限公司“東亞冷槽探索計劃(編號:20180101 )”項目聯合資助。
第一作者簡介:王照波,1971年生,男,高級工程師,主要從事地質礦產勘查、第四紀冰川與環境演化研究。
更新日期/Last Update: 2019-03-07
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