古地磁：从地球到火星

张伟杰; 盖聪聪; 柳加波; 姜兆霞; 刘青松

doi:10.3799/dqkx.2022.288

古地磁：从地球到火星

doi: 10.3799/dqkx.2022.288

张伟杰^1, ,,
盖聪聪¹,
柳加波^{1, 2},
姜兆霞³,
刘青松^{1, 2, 4, ,}

1.
南方科技大学海洋科学与工程系海洋磁学中心, 广东深圳 518055
2.
上海佘山地球物理国家野外科学观测研究站, 上海 201602
3.
中国海洋大学教育部深海圈层与地球系统前沿科学中心, 海底科学与探测技术教育部重点实验室和海洋地球科学学院, 山东青岛 266100
4.
南方海洋科学与工程广东省实验室(广州), 广东广州 511458

基金项目:

国家自然科学基金项目 41874078

国家自然科学基金项目 92158208

国家自然科学基金项目 42104068

国家自然科学基金项目 42176066

国家自然科学基金项目 41922026

深圳市科技计划资助 KQTD20170810111725321

博士后基金 2021M701557

自然资源部海洋地质与成矿作用重点实验室开放基金 MGM202003

同济大学海洋地质国家重点实验室开放基金 MGK202102

上海佘山地球物理国家野外科学观测研究站开放基金 SSKP202101

详细信息

作者简介:
张伟杰(1995-), 男, 博士研究生, 主要从事地磁场古强度研究.ORCID: 0000-0002-5586-918X.E-mail: 12031188@mail.sustech.edu.cn

通讯作者:
刘青松, E-mail: qsliu@sustech.edu.cn

中图分类号: P318
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- 被引次数: 0
出版历程
- 收稿日期: 2022-05-17
- 刊出日期: 2022-10-25

Paleomagnetism: From the Earth to Mars

Zhang Weijie^{1
,
,},
Gai Congcong¹,
Liu Jiabo^{1, 2},
Jiang Zhaoxia³,
Liu Qingsong^{1, 2, 4
, ,}

1.
Centre for Marine Magnetism (CM2), Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen 518055, China
2.
Shanghai Sheshan National Geophysical Observatory, Shanghai 201602, China
3.
Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, Ministry of Education, College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
4.
Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458, China

摘要

摘要: 古地磁学是一门典型的交叉学科，通过综合地质学、地球物理学、环境科学等学科相关方法，分析天然样品中记录的磁学信息，深入研究地磁场演化、地球动力学过程、古环境与古气候演化等.自20世纪中叶以来，古地磁学在各研究领域得到快速发展，通过进一步与其他学科交叉，衍生出诸多新兴方向.首先回顾了古地磁学的发展历史与基础研究领域.在此基础上，重点介绍了高精度卫星磁测与相关研究新领域、月球与火星磁学研究的新进展.同时，对古地磁学与高精度磁测等方法集成在地磁场演化、板块构造、深部结构、月球磁场演化、火星磁场及环境演化等方面的综合应用进行了讨论.最后，对古地磁学未来的潜在研究方向进行了展望.
- 古地磁学 /
- 卫星磁测 /
- 月球磁场 /
- 火星磁场 /
- 地磁学
Abstract: Paleomagnetism involves in interdisciplinary studies including geology, geophysics, and environmental science, etc..It focuses on geomagnetic field evolution, geodynamic process, paleoenvironment and paleoclimate evolution by analyzing magnetic information in natural samples.Since the mid-20th century, paleomagnetism has developed rapidly in various research fields, and many new research branches have been derived by integrating with other disciplines.In this paper, it firstly reviews the history and basic research fields of paleomagnetism.Then, it introduces the high-precision satellite magnetic survey and its related research fields, as well as new progress in the moon and mars magnetism.It further discusses the integrated applications of paleomagnetism, high-precision magnetic survey, and other methods in geomagnetic field evolution, plate tectonics, deep earth structure, Lunar and Martian magnetic field and environmental evolution.Finally, it proposes some potential research directions of paleomagnetism.
- paleomagnetism /
- satellite magnetic survey /
- moon magnetism /
- mars magnetism /
- geomagnetism

HTML全文

图 1 2020年全球地磁场强度分布图（数据来源于IGRF-13）

据Alken et al.（2021）

Fig. 1. Global geomagnetic intensity map (data from IGRF-13)

下载: 全尺寸图片幻灯片

图 2 全球岩石圈1 050阶球谐模型平均地球半径位置径向分量

据Thébault et al.（2021）

Fig. 2. Radial component of global lithosphere spherical harmonic model up to degree 1 050 at Earth's mean radius

下载: 全尺寸图片幻灯片

图 3 大洋磁异常（a~c）与沉积物相对古强度模拟得到的海洋磁异常（d）结果对比

据Li et al.（2021c）

Fig. 3. The oceanic magnetic anomalies (a-c) and the oceanic magnetic anomalies obtained from the simulation of the relative paleointensity of sediments (d)

下载: 全尺寸图片幻灯片

图 4 月球磁场强度演化

据Tikoo and Evans（2021）

Fig. 4. Evolution of Lunar magnetic field strength

下载: 全尺寸图片幻灯片

图 5 火壳厚度分布图

据Zuber（2001）

Fig. 5. Martian crust thickness map

下载: 全尺寸图片幻灯片

图 6 火星表面磁场径向分量

a.北极点俯视图；c.南极点仰视图. 据Langlais et al.（2019）

Fig. 6. Radial component of the magnetic field on the surface of Mars

下载: 全尺寸图片幻灯片

图 7 火星磁场发电机运行时间及可能模式

a. 海拉斯、阿尔及尔、伊希地负磁异常代表发电机停止；b. 海拉斯、阿尔及尔、伊希地负磁异常不代表发电机停止；c.“晚期”发电机

Fig. 7. Operating times and possible modes of the Mars magnetic dynamo

下载: 全尺寸图片幻灯片

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