大陆与地球系统的长期演化

IF 25.2 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Peter A. Cawood, Priyadarshi Chowdhury, Jacob A. Mulder, Chris J. Hawkesworth, Fabio A. Capitanio, Prasanna M. Gunawardana, Oliver Nebel
{"title":"大陆与地球系统的长期演化","authors":"Peter A. Cawood,&nbsp;Priyadarshi Chowdhury,&nbsp;Jacob A. Mulder,&nbsp;Chris J. Hawkesworth,&nbsp;Fabio A. Capitanio,&nbsp;Prasanna M. Gunawardana,&nbsp;Oliver Nebel","doi":"10.1029/2022RG000789","DOIUrl":null,"url":null,"abstract":"<p>Understanding of secular evolution of the Earth system is based largely on the rock and mineral archive preserved in the continental lithosphere. Based on the frequency and range of accessible data preserved in this record, we divide the secular evolution into seven phases: (a) “<i>Proto-Earth</i>” (ca. 4.57–4.45 Ga); (b) “<i>Primordial Earth</i>” (ca. 4.45–3.80 Ga); (c) “<i>Primitive Earth</i>” (ca. 3.8–3.2 Ga); (d) “Juvenile <i>Earth</i>” (ca. 3.2–2.5 Ga); (e) “<i>Youthful Earth</i>” (ca. 2.5–1.8 Ga); (f) “<i>Middle Earth</i>” (ca. 1.8–0.8 Ga); and (g) “<i>Contemporary Earth</i>” (since ca. 0.8 Ga). Integrating this record with knowledge of secular cooling of the mantle and lithospheric rheology constrains the changes in the tectonic modes that operated through Earth history. Initial accretion and the Moon forming impact during the Proto-Earth phase likely resulted in a magma ocean. The solidification of this magma ocean produced the Primordial Earth lithosphere, which preserves evidence for intra-lithospheric reworking of a rigid lid, but which also likely experienced partial recycling through mantle overturn and meteorite impacts. Evidence for craton formation and stabilization from ca. 3.8 to 2.5 Ga, during the Primitive and Juvenile Earth phases, likely reflects some degree of coupling between the convecting mantle and a lithosphere initially weak enough to favor an internally deformable, squishy-lid behavior, which led to a transition to more rigid, plate like, behavior by the end of the early Earth phases. The Youthful to Contemporary phases of Earth, all occurred within a plate tectonic framework with changes between phases linked to lithospheric behavior and the supercontinent cycle.</p>","PeriodicalId":21177,"journal":{"name":"Reviews of Geophysics","volume":null,"pages":null},"PeriodicalIF":25.2000,"publicationDate":"2022-12-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1029/2022RG000789","citationCount":"25","resultStr":"{\"title\":\"Secular Evolution of Continents and the Earth System\",\"authors\":\"Peter A. Cawood,&nbsp;Priyadarshi Chowdhury,&nbsp;Jacob A. Mulder,&nbsp;Chris J. Hawkesworth,&nbsp;Fabio A. Capitanio,&nbsp;Prasanna M. Gunawardana,&nbsp;Oliver Nebel\",\"doi\":\"10.1029/2022RG000789\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>Understanding of secular evolution of the Earth system is based largely on the rock and mineral archive preserved in the continental lithosphere. Based on the frequency and range of accessible data preserved in this record, we divide the secular evolution into seven phases: (a) “<i>Proto-Earth</i>” (ca. 4.57–4.45 Ga); (b) “<i>Primordial Earth</i>” (ca. 4.45–3.80 Ga); (c) “<i>Primitive Earth</i>” (ca. 3.8–3.2 Ga); (d) “Juvenile <i>Earth</i>” (ca. 3.2–2.5 Ga); (e) “<i>Youthful Earth</i>” (ca. 2.5–1.8 Ga); (f) “<i>Middle Earth</i>” (ca. 1.8–0.8 Ga); and (g) “<i>Contemporary Earth</i>” (since ca. 0.8 Ga). Integrating this record with knowledge of secular cooling of the mantle and lithospheric rheology constrains the changes in the tectonic modes that operated through Earth history. Initial accretion and the Moon forming impact during the Proto-Earth phase likely resulted in a magma ocean. The solidification of this magma ocean produced the Primordial Earth lithosphere, which preserves evidence for intra-lithospheric reworking of a rigid lid, but which also likely experienced partial recycling through mantle overturn and meteorite impacts. Evidence for craton formation and stabilization from ca. 3.8 to 2.5 Ga, during the Primitive and Juvenile Earth phases, likely reflects some degree of coupling between the convecting mantle and a lithosphere initially weak enough to favor an internally deformable, squishy-lid behavior, which led to a transition to more rigid, plate like, behavior by the end of the early Earth phases. The Youthful to Contemporary phases of Earth, all occurred within a plate tectonic framework with changes between phases linked to lithospheric behavior and the supercontinent cycle.</p>\",\"PeriodicalId\":21177,\"journal\":{\"name\":\"Reviews of Geophysics\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":25.2000,\"publicationDate\":\"2022-12-07\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://onlinelibrary.wiley.com/doi/epdf/10.1029/2022RG000789\",\"citationCount\":\"25\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Reviews of Geophysics\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://onlinelibrary.wiley.com/doi/10.1029/2022RG000789\",\"RegionNum\":1,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Reviews of Geophysics","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1029/2022RG000789","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 25

摘要

对地球系统长期演化的认识主要是基于保存在大陆岩石圈中的岩石和矿物档案。根据该记录中保存的可获得资料的频率和范围,我们将其长期演化分为7个阶段:(a)“原始地球”(约4.57-4.45 Ga);(b)“原始地球”(约4.45-3.80 Ga);(c)“原始地球”(约3.8-3.2 Ga);(d)“幼年地球”(约3.2-2.5 Ga);(e)“青年地球”(约2.5-1.8 Ga);(f)“中土世界”(约1.8-0.8 Ga);(g)“当代地球”(约0.8 Ga以来)。将这一记录与地幔长期冷却和岩石圈流变学的知识相结合,限制了贯穿地球历史的构造模式的变化。原始地球阶段的初始吸积和月球形成的冲击可能导致了岩浆海洋。岩浆海洋的凝固产生了原始地球岩石圈,它保留了岩石圈内部刚性盖子改造的证据,但也可能通过地幔翻转和陨石撞击经历了部分再循环。克拉通形成和稳定的证据大约在3.8至2.5 Ga之间,在原始和青少年地球阶段,可能反映了对流地幔和岩石圈之间的某种程度的耦合,最初足够弱,有利于内部变形,软盖行为,导致过渡到更刚性,板块样的行为,到早期地球阶段结束。地球的年轻到现代阶段,都发生在板块构造框架内,阶段之间的变化与岩石圈行为和超大陆旋回有关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Secular Evolution of Continents and the Earth System

Understanding of secular evolution of the Earth system is based largely on the rock and mineral archive preserved in the continental lithosphere. Based on the frequency and range of accessible data preserved in this record, we divide the secular evolution into seven phases: (a) “Proto-Earth” (ca. 4.57–4.45 Ga); (b) “Primordial Earth” (ca. 4.45–3.80 Ga); (c) “Primitive Earth” (ca. 3.8–3.2 Ga); (d) “Juvenile Earth” (ca. 3.2–2.5 Ga); (e) “Youthful Earth” (ca. 2.5–1.8 Ga); (f) “Middle Earth” (ca. 1.8–0.8 Ga); and (g) “Contemporary Earth” (since ca. 0.8 Ga). Integrating this record with knowledge of secular cooling of the mantle and lithospheric rheology constrains the changes in the tectonic modes that operated through Earth history. Initial accretion and the Moon forming impact during the Proto-Earth phase likely resulted in a magma ocean. The solidification of this magma ocean produced the Primordial Earth lithosphere, which preserves evidence for intra-lithospheric reworking of a rigid lid, but which also likely experienced partial recycling through mantle overturn and meteorite impacts. Evidence for craton formation and stabilization from ca. 3.8 to 2.5 Ga, during the Primitive and Juvenile Earth phases, likely reflects some degree of coupling between the convecting mantle and a lithosphere initially weak enough to favor an internally deformable, squishy-lid behavior, which led to a transition to more rigid, plate like, behavior by the end of the early Earth phases. The Youthful to Contemporary phases of Earth, all occurred within a plate tectonic framework with changes between phases linked to lithospheric behavior and the supercontinent cycle.

求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
Reviews of Geophysics
Reviews of Geophysics 地学-地球化学与地球物理
CiteScore
50.30
自引率
0.80%
发文量
28
审稿时长
12 months
期刊介绍: Geophysics Reviews (ROG) offers comprehensive overviews and syntheses of current research across various domains of the Earth and space sciences. Our goal is to present accessible and engaging reviews that cater to the diverse AGU community. While authorship is typically by invitation, we warmly encourage readers and potential authors to share their suggestions with our editors.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信