جزئیات کتاب
فرمت
جلد سخت
زبان
انگلیسی
منتشر شده
Jan 1, 1740
ناشر
Cambridge University Press
توضیحات
In this insightful exploration of planetary geology, readers are taken on a journey through the layers that compose the crusts of various celestial bodies. The author delves into the intricate processes that shape these surfaces, examining the mineralogical, chemical, and physical properties that define them. Through a captivating narrative, the complexities of crust formation are unraveled, revealing the interplay between various geological forces over time.
The book highlights the uniqueness of different planetary crusts, shedding light on how their origins and evolutionary paths differ throughout the solar system. By comparing terrestrial planets, moons, and other celestial bodies, the work emphasizes the diversity present in planetary crusts and encourages a deeper understanding of their significance in the broader context of planetary science.
Richly informative and meticulously researched, this volume serves as an essential resource for both students and professionals in the field. It provides a comprehensive overview of the current state of knowledge surrounding planetary crusts, making it a valuable addition to the literature on planetary science, geology, and planetary formation.
The book highlights the uniqueness of different planetary crusts, shedding light on how their origins and evolutionary paths differ throughout the solar system. By comparing terrestrial planets, moons, and other celestial bodies, the work emphasizes the diversity present in planetary crusts and encourages a deeper understanding of their significance in the broader context of planetary science.
Richly informative and meticulously researched, this volume serves as an essential resource for both students and professionals in the field. It provides a comprehensive overview of the current state of knowledge surrounding planetary crusts, making it a valuable addition to the literature on planetary science, geology, and planetary formation.