Mastodawn

The Origin Of Continents And Ocean Basins by M. V. Muratov

Professor Mikhail Muratov, P.Sc., Corr. Mem. USSR Acad. Sci., is Head of the Chair of Regional Geology and Paleontology, Moscow Institute of Geological Prospecting. He is the winner of State and Lenin Prizes.

This book deals with the origin, structure, and tectonic behavior of the earth’s crust beneath continents and oceans and describes principal stages of the earth’s geologic history. The author attaches much importance to geosynclinal cycles and their role in continental crust build-up and discusses intriguing hypotheses explaining the present day face of our planet.

Translated from the Russian by V. Agranat

You can get the book here and here.

Twitter: @MirTitles
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Preface

Chapter I. Structure and Age of the Earth’s Crust
Face of the Earth (9)
Continental and Oceanic Crust of the Earth (12)
Age of the Earth’s Crust (17)

Chapter II. Continental Crust
Inhomogeneity of the Structure (24)
Unconformities and Their Significance (30)
Evolution of Fold Areas and Formation of Platform Basement (33)

Chapter III. The Basic Component Parts of the Continents: Ancient Platforms and Fold Belts
The Importance of Ancient and Young Platforms in the Structure of Continents (36)
A Brief Outline of the Structure of Continents (36)
Constituent Elements of Ancient Platforms (40)
Fold Belts (41)

Chapter IV. The Structure and History of Geosynclinal Fold Areas
The Study of Geosynclines (48)
The Structure of Geosynclinal Fold Areas (50)
An Outline History of Geosynclinal Areas (52)
Main Stage (52)
Orogenic Stage (59)
Formations of Sedimentary and Volcanic Series of Geosynclinal Areas (61)
Differences in Ages of Geosynclinal Areas and in Formations of Troughs (69)
The Role of Intrusive Complexes in the Geosynclinal Cycle (73)
Geosynclinal Areas: Proliferous Sources of Valuable Minerals (79)
Two Principal Types of Geosynclinal Areas and Their Role in the Build-up of the Granitic-Metamorphic Layer of the Earth’s Crust (85)

Chapter V. Structure and History of the Basement of Ancient Platforms
Major Structural Units (87)
The Structure of Archean Massifs (88)
Proterozoic Fold Areas (90)
The Protosedimentary Cover of Ancient Platforms (94)
Outline History of the Basement of Ancient Platforms (95)
The Basement of Ancient Platforms: Mineral Resources (98)

Chapter VI. History of Fold Belts and Formation of the Basement of Young Platforms
Generation of the Riphean Basement of Major and Minor Belts (100)
Formation of the Paleozoic Basement of the Ural-Mongolia, Atlantic, and Arctic Belts (103)
History of the Mediterranean Fold Belt (106)
Inland Sea Basins and the Indonesia Area (108)
History of the Circum-Pacific Belt (112)
Formation of Granitic and Metamorphic Rocks of the Basement Within Fold Belts (124)

Chapter VII. Evolution of Ancient and Young Platforms
Basic Stages (127)
The Origin of Platform-Type Depressions (130)
Principal Valuable Minerals of the Sedimentary Cover of Platforms (132)
Volcanic Belts and Epiplatform Orogenesis (132)
Valuable Minerals in the Activated Areas of Platforms (134)

Chapter VIII. The Topography and Tectonics of the Ocean Floor
Principal Topographic Features and the Physiography (136)
Principal Tectonic Features of the Ocean Floor (140)
Pacific Ocean (140)
Indian Ocean (143)
Atlantic Ocean (144)
Arctic Ocean (147)

Chapter IX. The Origin of Ocean Basins in the Light of Geologic Evidence
The Physiography of the Pacific Bed and Its Probable Origin (149)
The Physiography of the Atlantic, Indian, and Arctic Beds and Their Origin (154)
Hypotheses Explaining the Conversion of Crustal Material Beneath the Ocean Floor (157)
Mobilistic Hypotheses Involving Continental Displacement (158)
Expanding Earth Hypothesis (165)
The Probable Age and the Mode of Formation of Ocean Basins (167)

Chapter X. Major Historical Events and the Stages of Formation of the Earth’s Crust
The Early Existence of the Earth Before Crust Formation (170)
The Basaltic Crust Before Hydrosphere Formation (170)
The Formation of the Granitic-Metamorphic Crust of Ancient Platforms (173)
The Consolidation of the Basement of Young Platforms (175)
The Latest Stage in the Development of the Earth’s Crust (177)
The General Trend in the Development of the Earth’s Crust (179)

Bibliography
Name Index
Subject Index

#1977 #geography #geologicalCycles #mirPublishers #oceanFloors #oceans #plateTectonics #sovietLiterature

Mir Books Oct 8

Terrestrial Oceans And Lunar Maria by G.F. Makarenko

About the Book
Both the Earth and the Moon have been repeatedly involved in episodes of volcanic activity induced by the heating of the interior of the two planets. Before the onset of each epoch of outpourings of lava that filled volcanic seas, arcuate and ring-shaped mountain chains encircled these seas in different regions of the planets.

The Moon is a “simplified model” of the Earth. Reviewing the structures of the Earth and the Moon simultaneously, we shall better understand the origins and compositions of the mountain ranges of the Pacific coast and see why the Atlantic-type oceans are not surrounded by mountains, and what is common in the structure of the volcanic floor of terrestrial oceans and lunar maria.

The book is intended for a wide circle of geologists, geographers, and astronomers and will also be of interest to those who are specializing in the geology of the Earth and the Moon.

About the Author

Galina Makarenko graduated from the Moscow Geological Exploration Institute named after Sergo Ordzhonikidse as an engineer-geologist. She is currently a member of the geological faculty at Moscow State University, where she conducts scientific research in the areas of geotectonics and volcanism. In addition to her research, she teaches general geology and trains both students and post-graduate students.
For many years, Makarenko participated in scientific expeditions in regions of ancient volcanism, with her candidate thesis dedicated to the geology of these areas. Her expeditions to Kamchatka and the Kuril Islands focused on comparing ancient volcanoes with active ones. Her doctoral thesis is centered on the extensive sheets of volcanic rocks found on the Earth’s continents and oceans.

She has published three monographs and numerous articles. Today, the author is actively engaged in collecting new data in the field of comparative planetology.

Translated from the Russian by

V.F. AGRANAT and V.F. POMINOV

You can get the book here and here.

Twitter: @MirTitles
Mastodon: @[email protected]
Mastodon: @[email protected]
Bluesky: mirtitles.bsky.social

Introduction 7

Earth: A Planet in a Basaltic Shell 11
A View of the Earth from Space 11
Mountains and Plains of Terrestrial Continents and Oceans 14
Volcanic Seas of Terrestrial Continents 22
Magma Melts Solidified at Depth 35
Basaltic Seas on Terrestrial Ocean Floors 40
Volcanic Rises on the Basaltic Ocean Floor 49
What Is Concealed by Lavas Lying on the Ocean Floor? 52

The Age of Terrestrial Basalts and Their Relationships with Different Structures 58
The Age of Trap Seas on the Continents 58
The Age of Volcanic Seas on the Ocean Floor 63
Volcanic Seas of Continents and Geosynclines 70
Volcanic Seas on the Ocean Floors and Island Arcs 81
Are Continental Basalts Similar to Oceanic Basalts on Earth? 88

Lava Maria on the Waterless Moon 93
The Distribution of Volcanic Maria 93
The Age of Lunar Basaltic Maria 102
Ridges and Grooves on the Floor of Lunar Maria 115
How Lunar Maria Were Formed? 120

Volcanic Maria of Planets Behind Arcuate Mountains 123
Volcanic Seas of the Earth and the Moon Have Similar Constitution 123
The Structures of the Earth and the Moon Are Symmetrical Relative to Their Axes of Rotation 131
Arcs and Rings of the Earth’s Oldest Mountains 135
The Centrifugal Wave in the Development of Mountain Arcs 147
The Moon Is a Simplified Model of the Earth 154

#earth #geology #lava #lavaFlow #moon #mountains #oceanFloors #plateTectonics #rocks #seas #sovietLiterature #valleys #volcanicSeas