热点如何形成火山链？
How does a hotspot form a volcano chain?
板块在固定热点上缓慢移动，先后形成的火山连成一串，如夏威夷岛链指示太平洋板块方向。
A plate drifts over a fixed hotspot, leaving a chain of volcanoes like the Hawaiian chain.
难度 专业 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#构造 #火山链
大陆漂移学说的主要内容是什么？
What is the main idea of continental drift?
魏格纳提出大陆曾连成一片（泛大陆），后分裂漂移。如今证据包括大陆轮廓吻合、相同化石跨洋分布。
Wegener proposed continents were once joined (Pangaea) and later split and drifted; evidence includes matching coastlines and identical fossils across oceans.
难度 专业 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#板块 #大陆漂移
什么是造山运动？
What is an orogeny?
造山运动是地壳因板块碰撞而强烈褶皱、断裂和抬升，形成山脉的地质过程，如阿尔卑斯造山。
Orogeny is the geologic process where crust folds, faults and uplifts strongly due to plate collisions, building mountains like the Alps.
难度 专业 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#板块 #造山运动
海沟是怎么形成的？
How do ocean trenches form?
在俯冲带，较重的大洋板块俯冲到另一板块之下，下沉弯曲形成深邃的海沟，如马里亚纳海沟。
At subduction zones a heavier oceanic plate dives beneath another, bending down to form deep trenches like the Mariana Trench.
难度 专业 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#板块 #海沟
地球磁场为什么会倒转？
Why does Earth's magnetic field reverse?
地核外核的液态铁镍对流不稳定，磁场偶极会减弱、混乱后重建为相反方向，平均数十万年发生一次。
The swirling iron-nickel outer core becomes unstable, the dipole weakens and rebuilds flipped, on average every few hundred thousand years.
难度 专业 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#地磁倒转 #地核
地幔对流到底是整层还是分层？
Is mantle convection whole-mantle or layered?
长期争论后，地震成像支持以全地幔对流为主，俯冲板片可沉入核幔边界，但部分地区存在滞留层。
Long debated, tomography now favors whole-mantle convection with slabs reaching the core-mantle boundary, though some regions show a stalled layer.
难度 专业 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#地幔对流 #全地幔
海底的"磁条带"是怎样证明海底扩张的？
How do magnetic stripes on the seafloor prove seafloor spreading?
洋中脊喷出的玄武岩含磁性矿物，冷却到居里点以下时按当时地磁场方向被磁化。地磁场历史上多次倒转，新洋壳持续记录每次倒转，于是洋中脊两侧形成对称的、正反相间的磁条带，像磁带一样。海底磁异常图显示条带年龄随离脊距离增大而变老，与海底扩张的预测完全吻合，成为板块构造最有力的证据之一，也间接证实了古地磁学预言的地磁倒转史。
Basalt erupting at mid-ocean ridges contains magnetic minerals that lock in the direction of Earth's field when they cool below the Curie point. Because the geomagnetic field has reversed many times, newly formed crust records each flip, leaving symmetric stripes of normal and reversed polarity on both flanks of the ridge, like a tape recording. Maps of seafloor magnetic anomalies show stripes getting older away from the ridge, exactly as seafloor spreading predicts—one of the strongest confirmations of plate tectonics and independent proof of the reversal history paleomagnetism had predicted.
难度 专业 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#磁条带 #地磁倒转 #海底扩张
什么是板块回卷？
What is slab rollback?
俯冲板片比周围地幔冷而重，负浮力把它往深处拖。当下拖快过汇聚供给的速率，海沟与随之迁移的岩浆弧便朝洋侧后退，这就是板片回卷。回卷在上覆板块后侧造出空间：弧被拉伸减薄、地幔上升减压熔融，于是形成弧后盆地，俯冲角与震源分布随之调整。但回卷并非弧后扩张的唯一原因，地幔对流与沿走向拖曳也能拉开弧后；两速消长时海沟会转为推进。
A subducting slab is colder and denser than the mantle around it, so its negative buoyancy drags it downward. When that pull outruns the rate at which convergence feeds plate into the trench, the trench and the magma arc attached to it migrate oceanward - that is slab rollback. Rollback opens space behind the upper plate: the arc is stretched and thinned, mantle rises and melts by decompression, a back-arc basin forms, and the dip of the slab and the distribution of its earthquakes adjust accordingly. Rollback is not the only way to open a back-arc basin, however, since mantle convection and trench-parallel drag can stretch it too; and when the two rates change balance, the trench turns from retreating to advancing.
难度 专业 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#构造 #回卷
什么是洋中脊？
What is a mid-ocean ridge?
洋中脊是沿张裂边界延伸的全球海底山系：地幔上涌减压熔融，玄武岩在两侧添成新洋壳，两翼年龄与地形对称，磁异常条带向外排开。它是世界最长的山链，足以把地球绕一圈还有余，却几乎全埋在深海之下，冰岛是少数露出海面的地段。两处易混：中脊未必在海盆正中，东太平洋海隆就偏在洋盆一侧；脊轴被横向转换断层错成一段段，断层本身不扩张。
A mid-ocean ridge is the global chain of submarine mountains built along divergent plate boundaries: as mantle rises it melts by decompression, and the basalt is added to both sides as new oceanic crust, so the flanks mirror each other in age and shape and the magnetic stripes spread symmetrically outward. It is the longest mountain chain on the planet, long enough to wrap the Earth more than once, yet nearly all of its axis lies deep beneath the sea, with Iceland one of the rare places where it breaks the surface. Two confusions to avoid: a mid-ocean ridge need not sit in the middle of its basin, since the East Pacific Rise lies off-centre in the Pacific; and its axis is stepped into segments by transverse transform faults, which do not spread themselves.
难度 专业 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#板块 #洋中脊
魏格纳提出大陆漂移时，有哪些证据支持他？
What evidence did Alfred Wegener marshal for continental drift?
魏格纳1912年提出大陆漂移说，依据包括：大西洋两岸海岸线形态吻合；巴西与西非的岩带和地层连续；舌羊齿植物群以及中龙、水龙兽等淡水生物化石跨洋分布；古冰川遗迹指向统一的冈瓦纳大陆冰盖；煤田、蒸发盐等古气候标志与现代纬度不符。这些几何、地层、生物、冰川和气候方面的证据，都指向各大陆曾连为一体。当时学界普遍反对，因为魏格纳没能提出令人信服的驱动力，直到20世纪60年代板块构造理论补上了机制，大陆漂移说才被重新接受。
In 1912 Wegener proposed continental drift, citing the jigsaw fit of Atlantic shorelines; continuous rock belts and strata across Brazil and West Africa; identical fossils on now-separated continents, including the Glossopteris flora and the freshwater reptiles Mesosaurus and Lystrosaurus; glacial striations implying a single Gondwana ice sheet; and paleoclimate markers such as coalfields and evaporites inconsistent with present latitudes. These geometric, stratigraphic, biologic, glacial, and climatic lines of evidence all pointed to formerly connected continents. Critics objected mainly because Wegener lacked a convincing driving force; only in the 1960s did plate tectonics supply the mechanism, and continental drift was finally vindicated.
难度 专业 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#大陆漂移 #魏格纳 #冈瓦纳
夏威夷火山链的年龄为什么从西北到东南越来越新？
Why are the Hawaiian volcanoes progressively younger toward the southeast?
夏威夷群岛上方的地幔热点固定在太平洋板块之下，来自地幔深处的热柱不断上涌提供岩浆，板块则向西北漂移，热点不断在新的位置"点燃"火山。于是西北端的火山最老、侵蚀最深，东南端的基拉韦厄火山最年轻、仍在喷发。热点火山链的方向和年龄梯度为板块运动的方向与速率提供了直接证据：考艾岛约500万年前喷发，而新火山活动延续至今。
A mantle hot spot sits fixed beneath the Pacific plate; a deep mantle plume feeds magma while the plate drifts northwest, so the plume lights volcanoes at new positions. The northwestern islands are therefore the oldest and most eroded, while Kilauea in the southeast is youngest and still erupting. The direction and age gradient of the chain give direct evidence of plate motion direction and speed: Kauai last erupted about 5 million years ago while the newest volcano is active today.
难度 专业 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#热点 #地幔柱 #夏威夷
像圣安德烈亚斯断层这样的转换边界是如何调节板块运动的？
How do transform boundaries such as the San Andreas Fault accommodate plate motion?
转换边界上两块板块水平错动、既不生成也不消亡地壳，圣安德烈亚斯断层便是太平洋板块与北美板块的右旋滑动边界。应力沿断层积累并周期性释放，造成浅源走滑型地震。
At a transform boundary two plates slide horizontally past each other without creating or destroying crust; the San Andreas Fault is the right-lateral boundary between the Pacific and North American plates. Stress builds along the fault and releases periodically in shallow strike-slip earthquakes.
难度 专业 · 适合 大众
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#转换断层 #圣安德烈亚斯 #走滑地震
板块运动怎样反过来改变全球气候？
How does plate tectonics feed back on global climate?
板块运动通过多种途径影响气候：造山带抬升加速硅酸盐风化，风化过程消耗大气二氧化碳并把碳埋入海洋，是长时间尺度的降温机制；巴拿马地峡的隆升切断了大西洋与太平洋的赤道洋流，可能促成北半球冰期；青藏高原与喜马拉雅的隆起强化亚洲季风，改变全球大气环流。这些板块尺度变化以千万年计，是驱动地质历史时期冷暖交替的重要因素。
Plate tectonics alters climate through several paths: mountain building accelerates silicate weathering, which consumes atmospheric CO2 and buries carbon in the ocean—a long-term cooling mechanism; the rise of the Isthmus of Panama cut off equatorial flow between the Atlantic and Pacific and likely helped trigger Northern Hemisphere glaciation; and uplift of the Tibetan Plateau and Himalaya intensified the Asian monsoon, reshaping global circulation. Operating on tens of millions of years, these tectonic changes are major drivers of deep-time climate swings.
难度 专业 · 适合 高中(15-18)
CC BY 4.0 · 来源待核验 · Source pending review
来源 · Source
出处备注：此条未指向带版次的可引用著作（通识性内容、机构文件或未展开的英文书名），本库不提供独立书目出处；如需精确引用，需由编辑补全具体篇目与版次。
Nature（板块构造与气候变化）
Nature (plate tectonics and climate change)
#板块-气候耦合 #硅酸盐风化 #青藏高原
什么是俯冲带？
What is a subduction zone?
密度大的大洋板块钻到另一板块之下沉入地幔的地方，常形成海沟和强烈地震火山。
Where a dense oceanic plate dives under another into the mantle, making trenches and quakes.
难度 进阶 · 适合 初中(12-15)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#构造 #俯冲带
大洋板块为什么会在海沟处沉入地幔？俯冲带能产生哪些现象？
Why does an oceanic plate sink into the mantle at a trench, and what happens along a subduction zone?
大洋板块比下面软流层的岩石更冷、更重、密度更大，于是会在海沟处像传送带一样弯折下沉进入地幔。俯冲板片在深处释放水分并诱发熔融，岩浆上升形成岛弧火山链，同时板片间的摩擦会引发频繁地震。著名的环太平洋火山地震带正是众多俯冲带拼接而成的。
Oceanic plates are colder, denser, and heavier than the asthenosphere below, so they bend and sink into the mantle at trenches like a conveyor belt. As the slab descends it releases water, triggering melting that feeds island-arc volcano chains, while friction between plates generates frequent earthquakes. The famous Pacific Ring of Fire is exactly a chain of such subduction zones.
难度 进阶 · 适合 初中(12-15)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#俯冲带 #海沟 #岛弧
板块移动得有多快？科学家是怎么量出来的？
How fast do tectonic plates move, and how do scientists measure it?
板块移动速度大致和指甲生长差不多，每年约2到10厘米，但持续几百万年就能累积成数千公里的位移。科学家用全球卫星定位系统（GPS）在固定于板块上的站点连续记录坐标，年复一年的微小变化就显示出板块的走向和速率，卫星测距与海底磁条带也相互印证。GPS测量让现代的大陆漂移从理论变成了可直接观察的现实。
Plates move at roughly the speed fingernails grow, about 2-10 cm per year, yet over millions of years that adds up to thousands of kilometers of displacement. Scientists use the Global Positioning System (GPS) to record coordinates at stations fixed on plates year after year; the tiny annual shifts reveal each plate's direction and speed, corroborated by satellite ranging and magnetic stripes on the seafloor. GPS measurements have turned continental drift from a theory into directly observable reality.
难度 进阶 · 适合 大众
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#板块运动 #GPS #大陆漂移
什么是威尔逊旋回？
What is the Wilson cycle?
它描述大洋从裂谷张开、扩宽、俯冲收缩到最终闭合的全过程，伴随大陆聚合与分裂的循环。
It describes an ocean's full life: rifting open, widening, subducting shut and finally closing, cycling continents together and apart.
难度 进阶 · 适合 大众
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#威尔逊旋回 #板块
地幔对流的驱动力是什么？板块运动与地幔对流有什么关系？
What drives mantle convection, and how does plate motion relate to it?
驱动力来自地幔内部的热：放射性元素衰变产热和地核向地幔底部的传热，使物质受热上升、冷却变密下沉。岩石圈板块正是对流圈顶部的冷边界层，在洋脊处新生、在俯冲处沉回地幔；现代观点认为俯冲板片的负浮力（板片拖拽）是板块运动的主要驱动力。
Convection is driven by internal heat—radiogenic decay and heat from the core—so material rises when hot and sinks when cooled and denser. Lithospheric plates are the cold boundary layer atop the convection cell, created at ridges and sinking back into the mantle at subduction zones; the modern view holds that the negative buoyancy of subducting slabs (slab pull) is the main driving force of plate motion.
难度 进阶 · 适合 大众
CC BY 4.0 · 已核验 · Verified 2026-10-03 · 2 条独立证据
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《普通地质学》(舒良树)
General Geology (Shu Liangshu)
独立核验依据 · Independent verification: 核验依据 2 DOUBAN ISBN 标识 9787116064911（按标识回读: 普通地质学）
#地幔对流 #板块运动 #板片拖拽
什么是俯冲带？为什么最深的海洋海沟都位于那里？
What is a subduction zone and why are the deepest ocean trenches found there?
俯冲带是密度较大的大洋板块俯冲到另一板块之下的边界，下插的板块把海床拉出深而窄的沟槽，如马里亚纳海沟。这里也是火山弧与特大地震的高发地。
A subduction zone is a boundary where a denser oceanic plate dives beneath another plate; the descending slab pulls the seafloor into a deep, narrow trench such as the Mariana Trench. These zones also host volcanic arcs and the planet's largest earthquakes.
难度 进阶 · 适合 小学高段(9-12)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
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舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#俯冲带 #海沟 #马里亚纳
喜马拉雅山为什么还在长高？
Why is the Himalaya still rising?
印度板块持续向北挤压欧亚板块，使地壳缩短增厚，山脉以每年几毫米速度抬升。
The Indian plate keeps pushing into the Eurasian plate, shortening and thickening the crust, lifting the range by a few millimeters per year.
难度 进阶 · 适合 初中(12-15)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
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舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#板块 #造山
洋中脊是海底的"新地壳工厂"，海底扩张到底是怎么发生的？
Mid-ocean ridges are called seafloor factories — how exactly does seafloor spreading work?
在洋中脊处，地幔上涌的熔岩沿裂隙喷出，冷却后形成新的玄武岩洋壳，把两侧更老的洋壳向两边推开。海底以每年约2到5厘米的速度扩张，与大西洋两岸逐年远离的趋势相符。洋壳在洋中脊新生、在俯冲带消亡，整个洋盆因此不断更新。
At a mid-ocean ridge, magma rising from the mantle erupts along the rift, cools into new basaltic crust, and pushes the older seafloor aside. Spreading proceeds at roughly 2-5 cm per year, matching the steady separation of the coasts on either side of the Atlantic. New crust forms at the ridge and old crust is consumed at subduction zones, so ocean basins continually renew themselves.
难度 进阶 · 适合 初中(12-15)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#洋中脊 #海底扩张 #板块构造
地中海为什么在不断缩小？
Why is the Mediterranean shrinking?
非洲板块向北挤欧亚板块，使地中海两侧的边界互相靠拢，盆地被一点点挤压变窄。
Africa pushes into Eurasia, squeezing the Mediterranean basin narrower over time.
难度 进阶 · 适合 初中(12-15)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#构造 #地中海
什么是转换断层？
What is a transform fault?
转换断层是两盘沿其走向只做水平剪切错动的板块边界，它常把洋中脊错断成一截一截，沿线地震浅、垂直升降小，既不造山也无深源地震。它容易被误认成普通走滑断层：真错动只发生在相邻两段洋中脊之间，脊外侧两盘其实同向移动，图上巨大的错距只是假象，并非实际位移量。圣安德烈斯断层就是把洋中脊的转换段延伸到大陆上的例子。
A transform fault is a plate boundary whose two sides only slide horizontally along its strike. It commonly cuts mid-ocean ridges into offset segments, and quakes along it are shallow with little vertical movement, so it builds no mountains and has no deep-focus earthquakes. It is easily mistaken for an ordinary strike-slip fault: real displacement happens only between two adjacent ridge segments, because outside them both sides move in the same direction, so the huge offset on a map is an appearance, not the actual amount of slip. The San Andreas fault is a ridge transform segment extended onto a continent.
难度 进阶 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#构造 #转换断层
板块运动的主要驱动力是什么？
What drives plate motion?
板块运动的背景是地幔对流，但推拽力多来自板块自身：冷而密的板片在海沟下沉，拖住后面的板块，即板片拖拽；洋中脊抬高，新洋壳沿重力向两侧滑出，即脊推。一般认为板片拖拽最强，故有长俯冲带的板块最快，每年数厘米，与指甲生长同量级。易混的是把对流当传送带直接拖着岩石圈：对流只管输运热量，直接做功的是重力，板底拖曳有时反成阻力。
Mantle convection sets the background, but the forces that move plates come mostly from the plates themselves: a cold, dense slab sinks at a trench and drags the plate behind it, which is slab pull, while the mid-ocean ridge stands high and the young crust slides gravitationally outward, which is ridge push. Slab pull is generally held to be the strongest, which is why plates with a long subduction zone at their edge move fastest, a few centimetres a year, the same order as fingernail growth. The confusion to avoid is treating convection as a conveyor belt that drags the lithosphere along: convection only carries heat, gravity does the direct work, and basal drag can even act as resistance.
难度 进阶 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#构造 #板块驱动
当两个大陆板块相撞时会发生什么？
What happens when two continental plates collide?
两个大陆板块密度相近、都不下沉，碰撞处岩石被挤压抬升，形成高大的褶皱山脉，如喜马拉雅山就是印度板块与欧亚板块碰撞的结果。这类边界常伴随强烈地震。
Because both continental plates have similar low density, neither subducts; instead the rock between them is squeezed and pushed upward into great folded mountain ranges. The Himalaya formed this way from the collision of the Indian and Eurasian plates, and such boundaries often produce strong earthquakes.
难度 进阶 · 适合 初中(12-15)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#大陆碰撞 #褶皱山脉 #喜马拉雅
地球历史上有过哪些超级大陆？
Which supercontinents existed in Earth history?
已知有哥伦比亚、罗迪尼亚、潘诺蒂亚和约3亿年前的泛大陆等，它们聚了又散，塑造了气候与生物分布。
Examples include Columbia, Rodinia, Pannotia and Pangaea about 300 million years ago; they assembled and broke up, reshaping climate and life.
难度 进阶 · 适合 大众
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#超级大陆 #泛大陆
为什么板块边界附近多火山和地震？
Why are volcanoes and earthquakes common near plate boundaries?
边界处板块相互挤压、张裂或错动，应力集中释放引发地震，岩浆也容易沿薄弱带上升喷发。
At boundaries plates collide, separate or slide, concentrating stress that triggers quakes and lets magma rise through weak zones.
难度 进阶 · 适合 初中(12-15)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#板块 #火山地震
科学家如何用GPS测量板块运动？
How do scientists measure plate motion with GPS?
在板块上布设连续观测站，精确记录点位毫米级位移，长期积累就能算出板块每年移动的速度和方向。
Permanent GPS stations record millimeter-level position changes; over years they reveal each plate's speed and direction of motion.
难度 进阶 · 适合 大众
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#GPS #板块运动
地幔柱与热点有什么关系？
How are mantle plumes and hotspots related?
地幔柱是从核幔边界上升的热物质柱，在岩石圈底部加热形成固定的热点，板块漂移时留下一串火山。
A mantle plume is a hot upwelling from deep mantle that heats a fixed hotspot at the base of the lithosphere, leaving a volcanic chain as plates drift.
难度 进阶 · 适合 大众
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#地幔柱 #热点
什么是地缝合线？
What is a suture zone?
当两个大陆相撞拼合，原先的大洋消失，留下的缝合带记录了这次碰撞，如喜马拉雅的雅鲁藏布缝合带。
Where colliding continents close an ocean, the leftover seam records the collision, e.g. the Indus suture.
难度 进阶 · 适合 高中(15-18)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#构造 #缝合带
东非大裂谷是怎么形成的？
How did the East African Rift form?
非洲板块内部受张裂应力拉薄地壳，形成一系列断裂谷地，未来可能演化成新海洋。
Inside the African plate, extensional stress thins the crust forming a chain of rift valleys that may become a new ocean in the future.
难度 进阶 · 适合 初中(12-15)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#板块 #裂谷
岩石圈和软流层有什么区别？为什么板块能"浮"在软流层上移动？
What is the difference between the lithosphere and the asthenosphere, and why can plates move across the asthenosphere?
岩石圈由地壳和地幔最顶部坚硬的一层组成，约一百多公里厚，整体是刚性的。软流层在岩石圈之下，温度接近岩石熔点，呈缓慢蠕动的塑性状态。板块就是一块块岩石圈，它们像大木筏一样在软流层上缓慢漂移，因为软流层虽然仍是固体，却能在长时间尺度上流动，既支撑又运送上方的板块。
The lithosphere is the rigid outer shell made of the crust plus the stiff top of the mantle, about 100 km thick or more. Beneath it lies the asthenosphere, where rock approaches its melting point and deforms by slow creep. Tectonic plates are pieces of lithosphere that drift like rafts across the asthenosphere, because that layer, though still solid, can flow over long timescales, supporting and carrying the plates above it.
难度 进阶 · 适合 初中(12-15)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#岩石圈 #软流层 #板块
地热资源是怎么来的？
Where does geothermal energy come from?
地球内部放射性衰变和残余热量使岩层升温，地下水循环受热形成温泉或干热岩，可被开发利用。
Radioactive decay and residual heat warm rocks inside Earth; circulating groundwater heated this way forms hot springs or hot dry rock usable as energy.
难度 进阶 · 适合 初中(12-15)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#板块 #地热
什么是地幔热点？
What is a mantle hotspot?
地幔深处有固定上升的热柱，岩浆穿过板块喷出形成火山，如夏威夷群岛。
A fixed plume of hot mantle rises and erupts through plates, forming volcanoes like Hawaii.
难度 入门 · 适合 初中(12-15)
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#构造 #热点
地球表面主要有几大板块？
How many major tectonic plates does Earth have?
通常分为六大主要板块：太平洋、欧亚、印度洋、非洲、美洲和南极洲板块，还有许多小板块。
Usually six major plates: Pacific, Eurasian, Indo-Australian, African, American and Antarctic, plus many smaller ones.
难度 入门 · 适合 大众
CC BY 4.0 · 已核验 · Verified 2026-08-23 · 2 条独立证据
来源 · Source
舒良树 主编,《普通地质学》第3版(曾获全国首届优秀教材一等奖)
Shu Liangshu ed., General Geology, 3rd ed. (winner of the 1st National Excellent Textbook Award)
独立核验依据 · Independent verification: 核验依据 2 ISBN 9787116123892（豆瓣书目条目: 普通地质学）
#板块 #板块构造