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標(biāo)題: Titlebook: Geological Evolution of the Earth During the Precambrian; Lazarus J. Salop Book 1983 Springer-Verlag Berlin Heidelberg 1983 Cambrian.Geolo [打印本頁(yè)]

作者: 諷刺文章    時(shí)間: 2025-3-21 17:13
書目名稱Geological Evolution of the Earth During the Precambrian影響因子(影響力)




書目名稱Geological Evolution of the Earth During the Precambrian影響因子(影響力)學(xué)科排名




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書目名稱Geological Evolution of the Earth During the Precambrian讀者反饋




書目名稱Geological Evolution of the Earth During the Precambrian讀者反饋學(xué)科排名





作者: ear-canal    時(shí)間: 2025-3-22 00:00
https://doi.org/10.1007/978-3-642-68684-9Cambrian; Geologie; Pr?kambrium; atmosphere; environment; evolution; formation; geology; history; isotope; sed
作者: Memorial    時(shí)間: 2025-3-22 02:31

作者: obeisance    時(shí)間: 2025-3-22 05:09
Geologic Synthesis,ities of geologic evolution of each of these units were pointed out. Some general problems of geologic (mainly tectonic) evolution ensuing from the analysis will be briefly outlined in this chapter. In the first place these are the cyclicity, tendency, and continuity (inheritance) of geologic processes.
作者: 疲憊的老馬    時(shí)間: 2025-3-22 11:58

作者: 散步    時(shí)間: 2025-3-22 13:17
Geological Evolution of the Earth During the Precambrian978-3-642-68684-9
作者: 散步    時(shí)間: 2025-3-22 17:38
Book 1983his early stage in the Earth‘s evolution at that time. Recently, this situation has completely changed, due to new methods of study of the older forma- tions, and due also to the refinement of some well-known methods, in particular of division, dating, and correlation of "silent" metamorphic strata.
作者: Diaphragm    時(shí)間: 2025-3-23 00:25

作者: 完全    時(shí)間: 2025-3-23 04:11
The Theoretical Analysis of Political Risk,below. The basement of the erathem is unknown. In many regions of the world the supracrustals and plutonic rocks are unconformably overlain by the Paleoprotozoic (Archeoprotozoic) greenstone strata, but their original relations are commonly masked by later thermal-tectonic processes.
作者: 填滿    時(shí)間: 2025-3-23 09:30

作者: 蚊帳    時(shí)間: 2025-3-23 11:51

作者: 專心    時(shí)間: 2025-3-23 16:01
https://doi.org/10.1057/9781137317421r the succession of occurrence and origin of rocks even within a relatively small area. The determination of synchroneity of events imprinted in rocks of different remote areas becames much more difficult. How is this problem to be solved?
作者: 錯(cuò)    時(shí)間: 2025-3-23 18:50
https://doi.org/10.1007/978-3-030-48622-8t formations and signify a new large stage in the history of the planet; the platform-geosynclinal stage (see below). The term “Archeoprotozoic” here proposed for the era (erathem) seems to be more suitable, for it has a pronunciation similar to the “Archean”, a widely accepted name.
作者: 2否定    時(shí)間: 2025-3-23 23:05

作者: Baffle    時(shí)間: 2025-3-24 03:35
The Paleoprotozoic (Archeoprotozoic),t formations and signify a new large stage in the history of the planet; the platform-geosynclinal stage (see below). The term “Archeoprotozoic” here proposed for the era (erathem) seems to be more suitable, for it has a pronunciation similar to the “Archean”, a widely accepted name.
作者: 四目在模仿    時(shí)間: 2025-3-24 09:38
https://doi.org/10.1057/9780230625464S.S.R. recommended attributing these rocks to the Lower Proterozoic, as is done in many other countries. In Canada it is recognized as the Aphebian, in Australia in most cases as the Nullaginian. Following the world stratotype of the erathem — the Karelian Supergroup — it can also be called the Karelian.
作者: Costume    時(shí)間: 2025-3-24 12:53
The Mesoprotozoic,S.S.R. recommended attributing these rocks to the Lower Proterozoic, as is done in many other countries. In Canada it is recognized as the Aphebian, in Australia in most cases as the Nullaginian. Following the world stratotype of the erathem — the Karelian Supergroup — it can also be called the Karelian.
作者: 挑剔小責(zé)    時(shí)間: 2025-3-24 16:51
years ago the Precambrian appeared as an uncertain and even mystic prelude to geologic evolution. Even the very name - Precambrian - means some indi- visible unit in the early history of the Earth, the beginning of which is poorly known. At the same time it was obvious that the Precambrian formation
作者: Defraud    時(shí)間: 2025-3-24 19:02
Labour Conventions and National Law,ich is much shorter than that of other principal units in a general scale of the Precambrian. Moreover, unlike other Precambrian eras and suberas, separated by diastrophic cycles, the Eocambrian is marked by a large orogeny only at its beginning, and its boundary with the Cambrian shows no traces of any important tectonic events.
作者: ingrate    時(shí)間: 2025-3-25 01:08
The Eocambrian (Vendian sensu stricto),ich is much shorter than that of other principal units in a general scale of the Precambrian. Moreover, unlike other Precambrian eras and suberas, separated by diastrophic cycles, the Eocambrian is marked by a large orogeny only at its beginning, and its boundary with the Cambrian shows no traces of any important tectonic events.
作者: 使隔離    時(shí)間: 2025-3-25 04:34

作者: 去世    時(shí)間: 2025-3-25 07:41
most Eocambrian (the Lower Vendian). The Epiprotozoic was recognized as an erathem (era) in the Precambrian in my paper in 1964 (Salop 1964). This erathem could also be called the Katangan or Adelaidean according to the typical strata of Equatorial Africa or Southern Australia.
作者: 令人發(fā)膩    時(shí)間: 2025-3-25 14:14
The Neoprotozoic,mmonly occur in the same localities, and sometimes build up common extensive rock sequences (complexes or supergroups). At the same time, they are also characterized by stratigraphic or angular unconformities, locally of significant magnitude; the intrusive magmatism also separates these sub-erathems at places.
作者: Budget    時(shí)間: 2025-3-25 18:12
The Epiprotozoic,most Eocambrian (the Lower Vendian). The Epiprotozoic was recognized as an erathem (era) in the Precambrian in my paper in 1964 (Salop 1964). This erathem could also be called the Katangan or Adelaidean according to the typical strata of Equatorial Africa or Southern Australia.
作者: sparse    時(shí)間: 2025-3-26 00:03

作者: saturated-fat    時(shí)間: 2025-3-26 03:10

作者: 偽造    時(shí)間: 2025-3-26 08:11

作者: Cumbersome    時(shí)間: 2025-3-26 10:26

作者: figurine    時(shí)間: 2025-3-26 13:23

作者: ULCER    時(shí)間: 2025-3-26 20:01
The Epiprotozoic,e termination of the Katangan orogeny of the first order (680–650 m.y.). Thus, the formations examined constitute a separate stage in geologic evolution of the planet and its duration ( ~ 350 m.y.) is more than that of the Paleozoic Era (330 m.y.). Nevertheless, this large Precambrian unit was not p
作者: 發(fā)怨言    時(shí)間: 2025-3-27 00:48
The Eocambrian (Vendian sensu stricto),r 680–650 m.y. and prior to the beginning of the Cambrian period, that is earlier than 570 m.y. The duration of the Eocambrian is thus 100–80 m.y., which is much shorter than that of other principal units in a general scale of the Precambrian. Moreover, unlike other Precambrian eras and suberas, sep
作者: 事情    時(shí)間: 2025-3-27 04:59
Geologic Synthesis,ities of geologic evolution of each of these units were pointed out. Some general problems of geologic (mainly tectonic) evolution ensuing from the analysis will be briefly outlined in this chapter. In the first place these are the cyclicity, tendency, and continuity (inheritance) of geologic proces
作者: 是貪求    時(shí)間: 2025-3-27 08:24
https://doi.org/10.1057/9781137317421 of those known have not been understood. Historical geology aims at deciphering these pages recorded in an unknown language, at reconstructing their general sequence and clarifying the contents of the buried pages. In reading these rock records geologists apply many different methods and theories t
作者: 600    時(shí)間: 2025-3-27 10:02

作者: chuckle    時(shí)間: 2025-3-27 14:11

作者: nocturnal    時(shí)間: 2025-3-27 21:09
https://doi.org/10.1057/9780230625464nsitional” units) but previous to termination of the Karelian orogeny that completed the Mesoprotozoic Era 2000–1900 m.y. ago. Thus the duration of the Era is ~ 800 m.y. Earlier in the U.S.S.R. the strata examined were assigned to the Middle Proterozoic. In 1979 the Stratigraphic Committee of the U.
作者: MUT    時(shí)間: 2025-3-27 23:00

作者: 冷淡一切    時(shí)間: 2025-3-28 05:34
e termination of the Katangan orogeny of the first order (680–650 m.y.). Thus, the formations examined constitute a separate stage in geologic evolution of the planet and its duration ( ~ 350 m.y.) is more than that of the Paleozoic Era (330 m.y.). Nevertheless, this large Precambrian unit was not p
作者: 修正案    時(shí)間: 2025-3-28 06:59

作者: 松緊帶    時(shí)間: 2025-3-28 10:59
The Content of International Labour Law,ities of geologic evolution of each of these units were pointed out. Some general problems of geologic (mainly tectonic) evolution ensuing from the analysis will be briefly outlined in this chapter. In the first place these are the cyclicity, tendency, and continuity (inheritance) of geologic proces
作者: recession    時(shí)間: 2025-3-28 17:58
Markus Ehrenmueller-Jenseno has the best claim to consideration as Ireland’s first investigative journalist, William O’Brien, later a prominent Parnellite MP and agrarian leader.. The advice was proffered in 1879 when O’Brien, then aged 26, was just emerging as the star reporter on Dublin’s . newspaper—and, of course, it was
作者: 館長(zhǎng)    時(shí)間: 2025-3-28 21:28
1572-6126 e approach to formal semantics of fuzzy controllers.Goguen categories extend the relational calculus and its categorical formalization to the fuzzy world. Starting from the fundamental concepts of sets, binary relations and lattices this book introduces several categorical formulations of an abstrac




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