標(biāo)題: Titlebook: Hadean Earth; T. Mark Harrison Book 2020 Springer Nature Switzerland AG 2020 Hadean Eon.Early Earth.Plate Tectonics.Planetary Habitabilty. [打印本頁] 作者: POL 時(shí)間: 2025-3-21 18:47
書目名稱Hadean Earth影響因子(影響力)
書目名稱Hadean Earth影響因子(影響力)學(xué)科排名
書目名稱Hadean Earth網(wǎng)絡(luò)公開度
書目名稱Hadean Earth網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Hadean Earth被引頻次
書目名稱Hadean Earth被引頻次學(xué)科排名
書目名稱Hadean Earth年度引用
書目名稱Hadean Earth年度引用學(xué)科排名
書目名稱Hadean Earth讀者反饋
書目名稱Hadean Earth讀者反饋學(xué)科排名
作者: 元音 時(shí)間: 2025-3-21 22:11 作者: enumaerate 時(shí)間: 2025-3-22 03:39 作者: 使人煩燥 時(shí)間: 2025-3-22 07:36 作者: superfluous 時(shí)間: 2025-3-22 11:20
Why Hadean?,he earliest division of geologic time. Since then, the meaning of Hadean evolved to describe the first roughly 500 million years of Earth history, which currently coincides with the period for which we have no macroscopic rock record. The premise of this book is that there are four avenues available作者: conquer 時(shí)間: 2025-3-22 15:05
Thermal Evolution Models,re initially?limited by technological impediments?and adoption of assumptions regarding the relationship between interior temperature and planetary heat loss?that narrowed possible solutions. Radically new proposals regarding both the latter issue and discontinuous transitions between modes of heat 作者: Sinus-Rhythm 時(shí)間: 2025-3-22 20:03 作者: 煩憂 時(shí)間: 2025-3-22 23:22 作者: Provenance 時(shí)間: 2025-3-23 03:30 作者: Neuropeptides 時(shí)間: 2025-3-23 06:10
Plate Boundary Interactions Through Geologic History,w that absence of evidence is not evidence of absence. Of special concern is that the Precambrian geologic record is likely biased to rock compositions most likely to resist deformation and thus exposure to erosion at newly rifted continental margins where loss to subduction erosion could occur. Thu作者: 樸素 時(shí)間: 2025-3-23 12:31
Hadean Jack Hills Zircon Geochemistry,f ratios of Hadean Jack Hills zircons show large heterogeneities indicating a major differentiation of the silicate Earth by 4.50?Ga. A possible consequence of this differentiation is the formation of continental crust of similar order to the present. Studies of mineral inclusions within Hadean zirc作者: 壓倒性勝利 時(shí)間: 2025-3-23 15:14
Proposed Sources of Hadean Zircons,crust. Numerous models have been proposed to explain these characteristics, including an origin similar to Icelandic rhyolites or lunar KREEP terranes, crystallization from mafic igneous rocks, formation in impact melts or sagduction, plate boundary and heat pipe tectonic environments, and multi-sta作者: Chagrin 時(shí)間: 2025-3-23 19:31 作者: 未成熟 時(shí)間: 2025-3-24 01:01
Morpho- and Chemo-Fossil Evidence of Early Life,xygenating photosynthesis, this relationship has been seen as evidence of past biologic activity. However, as metamorphic grade increases, kerogens are reacted to simpler hydrocarbons, ultimately yielding graphitic residues. The discovery of isotopically light carbon isotopes in microscopic graphite作者: 阻擋 時(shí)間: 2025-3-24 02:21
Collectanea,uably overreacting in overthrow of that model, the community quickly adopted the view that the first many hundreds of millions of years of Earth history had been too turbulent to leave any record. Shortly thereafter, the emergence of the large radius ion microprobe provided the tool needed to first 作者: SOW 時(shí)間: 2025-3-24 07:57
Book 2020e of liquid water. This new view leaves open the possibility that life could have emerged shortlyafter Earth accretion. The epistemic limitations under which the old paradigm persisted are closely examined. The book is principally designed as a monograph but has the potential to be used as a text fo作者: 推崇 時(shí)間: 2025-3-24 13:13 作者: Diverticulitis 時(shí)間: 2025-3-24 14:50 作者: Tremor 時(shí)間: 2025-3-24 22:51
https://doi.org/10.1007/978-3-540-74038-4ppear to require global silicate differentiation by 4.50?±?0.02?Ga billion years. Tungsten isotopic data from mantle rocks provides evidence of core formation by about 4.53?Ga and either very early isotopic isolation of silicate reservoirs or disturbance by a late chondritic veneer. Despite evidence作者: TEN 時(shí)間: 2025-3-25 01:50 作者: CRAB 時(shí)間: 2025-3-25 05:23
https://doi.org/10.1057/9781137455062 in equilibrium with olivine or differentiating magma sheets following large impacts into early basaltic crusts. The remarkable range of estimates of the growth history of continental crust reflects a number of influences but, generally speaking, earlier growth has been increasingly favored as new a作者: 符合國情 時(shí)間: 2025-3-25 10:32 作者: 流利圓滑 時(shí)間: 2025-3-25 15:11
Laz?r Vl?sceanu,Marian-Gabriel Hanceanf ratios of Hadean Jack Hills zircons show large heterogeneities indicating a major differentiation of the silicate Earth by 4.50?Ga. A possible consequence of this differentiation is the formation of continental crust of similar order to the present. Studies of mineral inclusions within Hadean zirc作者: 闖入 時(shí)間: 2025-3-25 18:15
Kilian Bizer,Sebastian Lechner,Martin Führcrust. Numerous models have been proposed to explain these characteristics, including an origin similar to Icelandic rhyolites or lunar KREEP terranes, crystallization from mafic igneous rocks, formation in impact melts or sagduction, plate boundary and heat pipe tectonic environments, and multi-sta作者: 巧思 時(shí)間: 2025-3-25 21:02 作者: 紳士 時(shí)間: 2025-3-26 03:09
Sarah B. M. Kraak,Paul J. B. Hartxygenating photosynthesis, this relationship has been seen as evidence of past biologic activity. However, as metamorphic grade increases, kerogens are reacted to simpler hydrocarbons, ultimately yielding graphitic residues. The discovery of isotopically light carbon isotopes in microscopic graphite作者: 被告 時(shí)間: 2025-3-26 04:42
and the Memory of the Shoah (1961–1967)uably overreacting in overthrow of that model, the community quickly adopted the view that the first many hundreds of millions of years of Earth history had been too turbulent to leave any record. Shortly thereafter, the emergence of the large radius ion microprobe provided the tool needed to first 作者: LOPE 時(shí)間: 2025-3-26 10:37
shortlyafter Earth accretion. The epistemic limitations under which the old paradigm persisted are closely examined. The book is principally designed as a monograph but has the potential to be used as a text fo978-3-030-46689-3978-3-030-46687-9作者: 不法行為 時(shí)間: 2025-3-26 16:03 作者: MAIZE 時(shí)間: 2025-3-26 17:58
http://image.papertrans.cn/h/image/420418.jpg作者: 假設(shè) 時(shí)間: 2025-3-26 22:15 作者: 注意 時(shí)間: 2025-3-27 02:07
978-3-030-46689-3Springer Nature Switzerland AG 2020作者: 沙草紙 時(shí)間: 2025-3-27 08:44
Why Hadean?,ing of that time included the possibility that our planet had forever existed in a quasi-steady state. By the later part of that century, it was broadly understood that Earth must have experienced a discrete origin but that?details of that event might never be discerned. The advent of radiometric da作者: 不合 時(shí)間: 2025-3-27 10:53
Thermal Evolution Models, with missteps related to as yet undiscovered physics or fundamentally incorrect assumptions. While the former is unavoidable, the latter amounts to self-inflicted wounds that may have forestalled scientific progress. Even in the absence of knowledge of initial conditions, linear mathematical relati作者: NIB 時(shí)間: 2025-3-27 14:09
Radionuclide Produced Isotopic Variations in Mantle Rocks,ryos during runaway accretion that occurred within 1–10?Ma of formation of the first solar system solids at 4.567?±?0.001?Ga. Both long- and short-lived radionuclides leave isotopic signatures in mantle rocks that bear on when and how the silicate Earth formed and differentiated. The longstanding vi作者: grotto 時(shí)間: 2025-3-27 21:47 作者: senile-dementia 時(shí)間: 2025-3-28 00:49
Models of Continental Growth and Destruction,ere is widespread agreement that plate tectonics has been doing just that for at least the past billion years. We also don’t fully understand the structure of the continental crust; popular layered models lack mechanisms to produce such structures or to recover them?following tectonic homogenization作者: CREST 時(shí)間: 2025-3-28 04:53
Plate Boundary Interactions Through Geologic History,plate tectonics from operating at 4.3?Ga, evidence that it was is indirect. Although subduction initiation is a robust feature of the modern plate tectonic system and we can calculate with some accuracy when oceanic lithosphere attains negative buoyancy, we don’t yet understand how strong the lithos作者: 令人發(fā)膩 時(shí)間: 2025-3-28 07:49 作者: Perineum 時(shí)間: 2025-3-28 11:48 作者: Intrepid 時(shí)間: 2025-3-28 18:01
Proposed Sources of Hadean Zircons,rologic observations of Hadean Jack Hills zircons. These are: (1) a zircon sub-population enriched in .O and depleted in .Si relative to mantle values; (2) low crystallization temperatures; (3) the presence of primary hydrous mineral inclusions; (4) the predominance of magmatic muscovite,?quartz, an作者: Preamble 時(shí)間: 2025-3-28 21:30
Could the Hadean Eon Have Been Habitable?,ns can provide some constraints. We are certain that life as we know it would not be possible without four requirements; soluble bioactive elements (carbon, hydrogen, oxygen, nitrogen, sulfur and phosphorous), free energy, liquid water, and time. Beyond these essential ingredients, there is broad ag作者: 嚴(yán)厲譴責(zé) 時(shí)間: 2025-3-29 01:10 作者: expunge 時(shí)間: 2025-3-29 07:06
Collectanea,arth history saw a desiccated, lifeless, molten wasteland is worthy of analysis. This chapter addresses problematic aspects of our epistemology that led to this paradigm and concludes that the historical sciences can sometimes be influenced by the same existential urges for control that fueled the p作者: 不適 時(shí)間: 2025-3-29 09:52 作者: 傲慢人 時(shí)間: 2025-3-29 11:26
Eric Magnus Campbell Tigerstedt, with missteps related to as yet undiscovered physics or fundamentally incorrect assumptions. While the former is unavoidable, the latter amounts to self-inflicted wounds that may have forestalled scientific progress. Even in the absence of knowledge of initial conditions, linear mathematical relati作者: reptile 時(shí)間: 2025-3-29 18:51
https://doi.org/10.1007/978-3-540-74038-4ryos during runaway accretion that occurred within 1–10?Ma of formation of the first solar system solids at 4.567?±?0.001?Ga. Both long- and short-lived radionuclides leave isotopic signatures in mantle rocks that bear on when and how the silicate Earth formed and differentiated. The longstanding vi作者: 故意釣到白楊 時(shí)間: 2025-3-29 22:03
From Institution to Self-regulationtest to conditions then extant in the inner solar system. The concept of a lunar cataclysm at?~3.9?Ga grew from seemingly contradictory observations of elemental fractionation in lunar highland rocks. U–Pb—and some Rb–Sr—data suggested recrystallization occurred between about 4.0 and 3.8?Ga. The Lat作者: labile 時(shí)間: 2025-3-30 01:56
https://doi.org/10.1057/9781137455062ere is widespread agreement that plate tectonics has been doing just that for at least the past billion years. We also don’t fully understand the structure of the continental crust; popular layered models lack mechanisms to produce such structures or to recover them?following tectonic homogenization
