南雄盆地晚白垩世&mdash;古新世陆源沉积组份变化的古气候指示

王尹; 李祥辉; 周勇; 刘玲

doi:10.14027/j.cnki.cjxb.2015.01.012

南雄盆地晚白垩世—古新世陆源沉积组份变化的古气候指示

doi: 10.14027/j.cnki.cjxb.2015.01.012

王尹^1,2,
李祥辉²,
周勇³,
刘玲¹

1.
江苏省有色金属华东地质勘查局八一四队南京 210007;
2.
南京大学地球科学与工程学院内生金属矿床成矿机制研究国家重点实验室南京 210093;
3.
四川省地质矿产勘查开发局四零二地质队成都 611730

基金项目: 国家自然科学基金项目(批准号:41372106)和国际重点基础研究发展计划“973”项目(编号:2012CB822003)联合资助

详细信息

作者简介:
王尹男 1985年出生硕士古气候与古土壤 E-mail: yin31721@qq.com

中图分类号: P532

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Paleoclimate Indication of Terrigenous Clastic Rock's Component during the Late Cretaceous-Early Paleocene in the Nanxiong Basin

1.
TEAM 814 East China Mineral Exploration and Development Bureau, Nanjing 210007;
2.
State Key Laboratory of Mineral Deposit Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210093;
3.
402th Geological Survey, Sichuan Bureau of Geology and Mineral Resources, Chengdu 611730

摘要

摘要: 利用陆源沉积中的碎屑组份(泥岩中的碎屑黏土矿物种类和砂岩中砂、粉砂碎屑类型)相对含量变化,对广东北部和江西南部的南雄盆地晚白垩世—古新世古气候进行了分析.结果显示,砂岩碎屑组份含量气候指数(长石/石英比,F/Q)介于0.02~0.14之间;(碎屑)黏土矿物组合主要以伊利石为主,平均79%;伊利石结晶度指数与化学指数分别为0.25~0.39、0.31~0.7.进一步分析表明,研究区这一时期以干旱气候为主,存在暖湿气候间断,古气候演化可分为三个阶段:晚白垩世马斯特里赫特期以干旱—半干旱性气候为主,古新世丹尼期早期转变为相对湿热或与干旱—半干旱气候交替,古新世丹尼期晚期恢复到半干旱性气候,但比第一阶段湿度可能稍有增加.这一总体干旱—半干旱气候格局及其变化总体与同期全球气候变化一致.
- 碎屑组份指针 /
- 黏土矿物 /
- 古气候 /
- 晚白垩世 /
- 古新世 /
- 南雄盆地
Abstract: According to relative content of terrigenous clastic rock's components (clay minerals of claystone and clastic composition of sandstone), analyzing paleoclimate of Late Cretaceous - Paleocene Nanxiong Basin in northern Guangdong and southern Jiangxi. The climate index of sandstone clastic components (feldspar/quartz, F/Q) is between 0.02 to 0.14; Clay mineral assemblage is mainly illite, with an average of 79%; Illite crystallinity index and chemical index is 0.25~0.39 and 0.31~0.7. During this period, the climate of the study area is mainly arid climate, with some warm and humid climate intermittent, paleoclimate can be divided into three stages: arid-semiarid Maastrichtian, warm and moist semiarid early Danian, and the semiarid late Danian. Climate evolution is consistent with the same period of global climate change.
- F/Q ratio /
- clay mineral /
- paleoclimate /
- Late Cretaceous /
- Paleocene /
- Nanxiong Basin

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参考文献(66)

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南雄盆地晚白垩世—古新世陆源沉积组份变化的古气候指示

doi: 10.14027/j.cnki.cjxb.2015.01.012

作者简介:
王尹男 1985年出生硕士古气候与古土壤 E-mail: yin31721@qq.com

计量

Paleoclimate Indication of Terrigenous Clastic Rock's Component during the Late Cretaceous-Early Paleocene in the Nanxiong Basin

计量

目录

南雄盆地晚白垩世—古新世陆源沉积组份变化的古气候指示

doi: 10.14027/j.cnki.cjxb.2015.01.012

1. 江苏省有色金属华东地质勘查局八一四队南京 210007;

2. 南京大学地球科学与工程学院内生金属矿床成矿机制研究国家重点实验室南京 210093;

3. 四川省地质矿产勘查开发局四零二地质队成都 611730

作者简介:
王尹男 1985年出生硕士古气候与古土壤 E-mail: yin31721@qq.com

English Abstract

Paleoclimate Indication of Terrigenous Clastic Rock's Component during the Late Cretaceous-Early Paleocene in the Nanxiong Basin

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期刊在线

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南雄盆地晚白垩世—古新世陆源沉积组份变化的古气候指示

doi: 10.14027/j.cnki.cjxb.2015.01.012

作者简介: 王尹 男 1985年出生 硕士 古气候与古土壤 E-mail: yin31721@qq.com

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Paleoclimate Indication of Terrigenous Clastic Rock's Component during the Late Cretaceous-Early Paleocene in the Nanxiong Basin

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出版历程

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南雄盆地晚白垩世—古新世陆源沉积组份变化的古气候指示

doi: 10.14027/j.cnki.cjxb.2015.01.012

1. 江苏省有色金属华东地质勘查局八一四队 南京 210007; 2. 南京大学地球科学与工程学院内生金属矿床成矿机制研究国家重点实验室 南京 210093; 3. 四川省地质矿产勘查开发局四零二地质队 成都 611730

作者简介: 王尹 男 1985年出生 硕士 古气候与古土壤 E-mail: yin31721@qq.com

English Abstract

Paleoclimate Indication of Terrigenous Clastic Rock's Component during the Late Cretaceous-Early Paleocene in the Nanxiong Basin

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
王尹男 1985年出生硕士古气候与古土壤 E-mail: yin31721@qq.com

1. 江苏省有色金属华东地质勘查局八一四队南京 210007;

2. 南京大学地球科学与工程学院内生金属矿床成矿机制研究国家重点实验室南京 210093;

3. 四川省地质矿产勘查开发局四零二地质队成都 611730

作者简介:
王尹男 1985年出生硕士古气候与古土壤 E-mail: yin31721@qq.com