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High obliquity, high angular momentum Earth as Moon's origin revisited by Advanced Kinematic Model of Earth-Moon System

机译：高倾斜，高角动量地球作为月球原产地通过高级运动模型重新审视地球系统

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Bijay Kumar Sharma;
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1. Creating an isotopically similar Earth-Moon system with correct angular momentum from a giant impact [J] . Wyatt Bryant M., Petz Jonathan M., Sumpter William J., Journal of Astrophysics and Astronomy . 2018,第2期

机译：从巨大影响创造一个具有正确角动量的同位素类似的地球系统
2. Resonance in the perturbations of a synchronous satellite due to angular rate of the earth-moon system around the sun and the earth’s rotation rate [J] . Sushil Yadav, Rajiv Aggarwal, Bhavneet Kaur International Journal of Advanced Astronomy . 2016,第2期

机译：由于地球绕月系统在太阳周围的角速度和地球的旋转速度而引起的同步卫星摄动共振
3. Tidal evolution of the Moon from a high-obliquity, high - angular - momentum Earth [J] . Cuk Matija, Hamilton Douglas P., Lock Simon J., Nature . 2016,第7629期

机译：高倾角高角动量地球的潮汐演变。
4. Earth-Moon System; The Origin, Development and the Future. Mathematical-Physical Basics to the Computer Symulation of the System [C] . Tadeusz TUMALSKI 8th World Multi-Conference on Systemics, Cybernetics and Informatics(SCI 2004) vol.2: Computing Techniques . 2004

机译：地月系统；起源，发展与未来。系统计算机对称的数理基础
5. Characteristics and Design Strategies for Near Rectilinear Halo Orbits Within the Earth-Moon System [D] . Zimovan, Emily M. 2017

机译：月球系统内近直线晕轨道的特性和设计策略
6. The past and present Earth-Moon system: the speed of light stays steady as tides evolve [O] . James G Williams, Slava G Turyshev, Dale H Boggs -1

机译：过去和现在的地球-月亮系统：随着潮汐的发展光速保持稳定
7. Creating an Isotopically Similar Earth-Moon System with Correct Angular Momentum from a Giant Impact [O] . Wyatt, Bryant M., Petz, Jonathan M., Sumpter, William J., 2016

机译：创建具有正确角度的同位相似地月系统来自巨大影响的动力
8. Orbital, Rotational and Climatic Interactions: Energy Dissipation and Angular Momentum Exchange in the Earth-Moon System [R] . Egbert, Gary D. 2001

机译：轨道，旋转和气候相互作用：地月系统中的能量耗散和角动量交换

High obliquity, high angular momentum Earth as Moon's origin revisited by Advanced Kinematic Model of Earth-Moon System

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