The homogenization temperature in the fluid inclusions of Ordovician halite and paleoclimatic implication

被引：3

作者：

HU Bin ^{[1
,2
]}

KONG Fanjing ^{[1
,2
]}

ZHANG Yongsheng ^{[1
,2
]}

ZHENG Mianping ^{[1
,2
]}

CHEN Jing ^{[1
]}

机构：

[1] Institute of Mineral Resources, Chinese Academy of Geological Sciences

[2] Key Laboratory of Saline Lake Resources and Environments,Ministry of Land and Resources

来源：

Acta Geologica Sinica(English Edition) | 2014年 / S1期

关键词：

Fluid inclusions in halite; homogenization temperature; cooling nucleation method; halite of Northern Shaanxi Basin in Ordovician; paleoclimate;

D O I：

暂无

中图分类号：

P534.42 [奥陶纪（系）]; P532 [古气候学];

学科分类号：

070903 ;

摘要：

1 Introduction The homogenization temperature of fluid inclusions reflects the temperatures of the brines from which halite crystals grew.Therefore,it is a powerful mean to reveal the paleoclimate.Northern Shaanxi Salt Basin is located in the central and eastern of Ordos Basin.We have detail petrographical research and the homogenization

引用

页码：10 / 11

页数：2

共 3 条

[1]

Low-latitude Ordovician to Triassic brachiopod habitat temperatures (BHTs) determined from δ 18 O[brachiopod calcite] : A cold hard look at ice-house tropical oceans[J] . Peter S. Giles.Palaeogeography, Palaeoclimatology, Palaeoecology . 2012

[2]

Paleotemperatures from fluid inclusions in halite: method verification and a 100,000 year paleotemperature record, Death Valley, CA[J] . Tim K. Lowenstein,Jianren Li,Christopher B. Brown.Chemical Geology . 1998 (3)

[3] PALEOTEMPERATURES PRESERVED IN FLUID INCLUSIONS IN HALITE [J].

ROBERTS, SM ;

SPENCER, RJ .

GEOCHIMICA ET COSMOCHIMICA ACTA, 1995, 59 (19) :3929-3942

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