海洋地质与第四纪地质最新文献_第10页

LITHOSTRATIGRAPHIC CORRELATION OF MESOZOIC AND PALAEOZOIC MARINE STRATA BETWEEN SOUTH YELLOW SEA AND UPPER YANGTZE REGION 南黄海与上扬子地区中、古生代海相岩石地层对比

Marine Geology & Quaternary Geology Pub Date : 2013-01-01 DOI: 10.3724/sp.j.1140.2013.01109

Guo Xing-wei

引用次数: 13

STUDY OF POSITIVE INVERSION STRUCTURES IN THE NORTH DEPRESSION OF THE SOUTH YELLOW SEA BASIN 南黄海盆地北部坳陷正反转构造研究

Marine Geology & Quaternary Geology Pub Date : 2013-01-01 DOI: 10.3724/SP.J.1140.2013.03095

Nan Li, Weiran Li, Haiyan Long

引用次数: 2

Geochemical Responses to PALAEOCLIMATE:EVIDENCE from the Early-Mid Holocene Lake Deposits at Dishaogouwan Section in the Salawusu Catchment of Inner Mongolia 地球化学对古气候的响应——来自内蒙古萨拉乌苏流域早-中全新世底邵沟湾剖面湖泊沉积物的证据

Marine Geology & Quaternary Geology Pub Date : 2013-01-01 DOI: 10.3724/SP.J.1140.2013.040103

Qi Zhao, R. Fan, Bao-sheng Li, Mischke Steffen, Cheng-jun Zhang

{"title":"Geochemical Responses to PALAEOCLIMATE:EVIDENCE from the Early-Mid Holocene Lake Deposits at Dishaogouwan Section in the Salawusu Catchment of Inner Mongolia","authors":"Qi Zhao, R. Fan, Bao-sheng Li, Mischke Steffen, Cheng-jun Zhang","doi":"10.3724/SP.J.1140.2013.040103","DOIUrl":"https://doi.org/10.3724/SP.J.1140.2013.040103","url":null,"abstract":"Sediment grain size,organic carbon content(TOC),carbonate content and stable carbon and oxygen isotopes of carbonates in the Dishaogouwan section on the south edge of the Mu Us desert in Inner Mongolia were sludied in this paper.Age data were used to establish an age model for this section.All the sedimentary and geochemical paleoenvironmental proxies were used to reconstruct the palaeoenvironmental changes since 11 000 aBP,to 4 380 aBP,early to mid Holocene in this area.During the period from 11 000 aBP to 9 950 aBP,the study area was cool and dry.Precipitation in the south north part of Shanxi Loess Plateau and the water from melted Dishaogouwan frozen stratum were the main replenishment water for the Salawusu cathment.During the period of 9 950~9 100 aBP of early Holocene,temperature and precipitation increased with a high effective humidity,and the Dishaogouwan lake came into being.From 9 100 aBP to 5 850 aBP,temperature and precipitation continued to increase but effective humidity was a little lower,while the lake developed to its maximum and lasted for a long time.From 5 850 aBP to 5 100 aBP,temperature and precipitation started decreasing and the lake shrank at the same time.From 5 100 aBP to 4 700 aBP,palaeodune formed in this area under dry climate.There was a short period of temperature and rainfall rising during 4 500~4 380 aBP,and a small lake formed over a carbonate impermeable layer.Desertification has prevailed under the dry condition since 4 380 aBP up to present.","PeriodicalId":18188,"journal":{"name":"Marine Geology & Quaternary Geology","volume":"33 1","pages":"103"},"PeriodicalIF":0.0,"publicationDate":"2013-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69773421","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 1

RECORDS OF TERRIGENOUS DUST IN LACUSTRINE SEDIMENTS FROM DONGDAO ISLAND,SOUTH CHINA SEA 南海东岛湖相沉积物中陆源粉尘的记录

Marine Geology & Quaternary Geology Pub Date : 2013-01-01 DOI: 10.3724/SP.J.1140.2013.03001

Yi Liu, Liguang Sun, Yuhan Luo, Song Sun, Yuhong Wang

{"title":"RECORDS OF TERRIGENOUS DUST IN LACUSTRINE SEDIMENTS FROM DONGDAO ISLAND,SOUTH CHINA SEA","authors":"Yi Liu, Liguang Sun, Yuhan Luo, Song Sun, Yuhong Wang","doi":"10.3724/SP.J.1140.2013.03001","DOIUrl":"https://doi.org/10.3724/SP.J.1140.2013.03001","url":null,"abstract":"A lacustrine sediment core(DY6) was collected from the \"Nietang Pond\" on Dongdao Island,South China Sea(SCS).Geochemical,morphological,and mineralogical analyses were performed for the sediment samples.The results of major elements showed that the concentrations of Ti and Al in the sediment samples were much higher than those in three end-members(coral sand,guano and plants).Hierarchical clustering analysis of geochemical elements indicated that Al and Ti were exogenetic.Furthermore,according to the microscopic analysis,there are more acid-insoluble particles in the subsamples with high Ti(Al) contents,some of which showed similar morphological characters with the eolian dusts from Hefei,the loess-paleosol particles from Korea and the dust deposits from the north of SCS.The major elements concentrations of the acid-insoluble particles surfaces detected by X-ray energy spectrum revealed that these particles were mainly made up of silicate and quartz.Consequently,the accumulation of Ti and Al in the lacustrine sediments of Dongdao Island was quite possibly caused by the input of the terrigenous dust from the interior of Asia continent.The East Asian Winter Monsoon might be the transportation medium.","PeriodicalId":18188,"journal":{"name":"Marine Geology & Quaternary Geology","volume":"33 1","pages":"1"},"PeriodicalIF":0.0,"publicationDate":"2013-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69773578","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 4

SEDIMENTARY ENVIRONMENTAL EVOLUTION OF NINGSHAO PLAIN SINCE LAST GLACIAL MAXIMUM 末次盛冰期以来宁绍平原沉积环境演化

Marine Geology & Quaternary Geology Pub Date : 2013-01-01 DOI: 10.3724/SP.J.1140.2013.03037

Rui Liu, J. Qin

引用次数: 4

Evolution of Cenozoic Tethys and its Environmental Effects on Inland Drought 新生代特提斯的演化及其对内陆干旱的环境影响

Marine Geology & Quaternary Geology Pub Date : 2013-01-01 DOI: 10.3724/SP.J.1140.2013.040135

Donghuai Sun, Xin Wang, Baofeng Li, Fahu Chen, Fei Wang, Zaijun Li, Baiqing Liang, Zhiwei Ma

{"title":"Evolution of Cenozoic Tethys and its Environmental Effects on Inland Drought","authors":"Donghuai Sun, Xin Wang, Baofeng Li, Fahu Chen, Fei Wang, Zaijun Li, Baiqing Liang, Zhiwei Ma","doi":"10.3724/SP.J.1140.2013.040135","DOIUrl":"https://doi.org/10.3724/SP.J.1140.2013.040135","url":null,"abstract":"The evolution and extinction of the Tethys was a major global geological event in Cenogoic and is one of the decisive influences on the formation and evolution of the arid environment in Eurasia,especially Asia.This paper briefly made a review of the progress of the international Tethys programs,combined with our researches.The evolution of the Tethys can be simply divided into three stages,the Tethys,Paratethys and Tethys extinction.In Late Mesozoic to early Cenozoic,most parts of Europe,Western and Central Asia region and the Southern Tibetan Plateau joined together and formed an inland sea named the Tethys which connected with the Atlantic Ocean to the west and with the Ceno-Tethys to the east.About 34 Ma ago,The Tethys connected with the Atlantic,Indian and Arctic oceans and the most eastern part of it extended into the Tarim area.With the collision of Indian and Eurasian plates,the Tethys retreated from the Southern Tibetan Plateau and the Tarim area.Then the Tethys was separated into the Mediterranean in the south and Paratethys in the north about 34 Ma ago.Under the joint effect of global sea level change,tectonic uplift,surface erosion and sediment filling,the Parathtys experienced a series of eustatic,and area changes and closing and opening of seawater channels,The greatest impact on the environment came from the channel closing-opening of the Paratethys,the ancient Mediterranean and the Indian Ocean.Since Oligocene there occurred at least four times of close-open cycles.The evolution and extinction of the Tethys especially since the withdraw of Tethys from the Tarim region 34 Ma,the rapid shrinkage of Tethys about 20 Ma and the closing of water channels with other oceans around 7-8 Ma may be the main factors leading to the drying up in Asian inland area.","PeriodicalId":18188,"journal":{"name":"Marine Geology & Quaternary Geology","volume":"33 1","pages":"135"},"PeriodicalIF":0.0,"publicationDate":"2013-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69773850","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 3

The Vegetation Chenges in Ulan Buh Desert Since the Last GLACIAL:POLLEN Evidence from Core WL10ZK-1 末次冰期以来乌兰布和沙漠的植被Chenges:来自WL10ZK-1岩心的花粉证据

Marine Geology & Quaternary Geology Pub Date : 2013-01-01 DOI: 10.3724/SP.J.1140.2013.040169

Xuemei Chen, Guoqiang Li, Xiao-zhong Huang, Hui Zhao

引用次数: 2

DISTRIBUTION PATTERN OF HEAVY METALS IN THE SURFACE SEDIMENTS AND ENVIRONMENT QUALITY EVALUATION FOR THE YANGTZE RIVER DELTAIC ECONOMIC ZONE 长江三角洲经济区表层沉积物重金属分布格局及环境质量评价

Marine Geology & Quaternary Geology Pub Date : 2013-01-01 DOI: 10.3724/SP.J.1140.2013.05063

Shanshan Liu, Yong Zhang, Shuyun Gong, Kaining Yu, Ma Lin, Shipu Bi

引用次数: 4

The Influence of Magmatic Process and Hydrothermal Alteration on the Geochemical Characteristics of Abyssal Peridotites 岩浆作用和热液蚀变对深海橄榄岩地球化学特征的影响

Marine Geology & Quaternary Geology Pub Date : 2013-01-01 DOI: 10.3724/SP.J.1140.2013.05073

Zhiqiang Chen, Huaiyang Zhou, H. Yao, Yang Liu, Qunhui Yang, Jiejin Li, Jiwei Li, Zhilei Sun

引用次数: 0

BEACH EROSION ALONG THE COAST OF SHANDONG PROVINCE AND PROTECTION COUNTERMEASURES 山东沿海滩涂侵蚀及保护对策

Marine Geology & Quaternary Geology Pub Date : 2013-01-01 DOI: 10.3724/SP.J.1140.2013.05035

Guangxue Li, L. Gong, Jichao Yang, Dong Ding, Bin Li, Li-hua Cao, Yonghong Wang, Ling Liu

引用次数: 7