* Z8 Y- Y/ h& D* U3 j

& Q# t, H. [% Q6 g3 B& ] 1 / X! {9 r+ U5 F4 L$ v" |2 D
盘古大陆分裂和大陆漂移
4 [/ E* C" D9 |3 `: ]+ ~ 
4 I' o% r* y/ w# S0 V- ?: I 2
5 c/ X0 p" D4 G 大陆 - 海洋俯冲带
- H3 |2 O$ P2 M0 {2 S6 g R8 O" z2 z  8 v* W% F$ q2 x. s* P! q
3
: | Y8 j9 y, k9 P5 ?1 s/ F 印度 - 亚洲大陆碰撞 0 D2 Z: i! K) ]1 k, ?6 O9 c/ T
 fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E) % |/ d, D0 U$ Q* p1 K
4
% b T9 g _7 d$ V. O 南太平洋的形成 ' j* J1 y: ?0 B% A* r# {1 C! }
 fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E)
) G, q7 ~5 u+ O. Z$ h2 _6 |3 q 5 0 u& x4 ~8 I. b1 x% }0 N
海底扩张和海洋磁异常
' b0 b' e8 A2 F% R2 ~3 J+ L% O  fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E) 6 ~. I5 L. J; { H! k# Q
 fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E)
- q9 b5 y6 P8 M- H# H( n  fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E) 6 _/ r2 o2 q, q9 h
 fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E) ( W/ J; H- ?& y. u$ _ H
 fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E) + {* }0 w6 M7 O
6 6 M. O( o; I, L! B
加拿大冰盖和海岸线移动
! c4 C- F* o/ N5 k0 F6 _# z  fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E) % y3 ^7 ~* @4 F! J2 r
 fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E) 9 h/ |4 g/ _" F0 W3 f1 E
 fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E)
: R! Y, P8 f, R, [! j m9 B7 c  fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E)
9 b' t% w7 j* l c- P& v0 b: S 7 # s$ U1 \1 M0 m% N) x: e% T/ m4 A
沿海侵蚀与海洋梯田的形成 8 M* C' B4 I0 j6 r; D
 fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E) 7 v$ ]0 B0 I Q# r
 fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E) 2 I# Z4 q( X$ o# {; o2 x3 F7 Q
8 # Y1 I# U( ^. [
通过海底扩张形成的南太平洋 & \& }; `; M' R" c+ i' s
 fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E)
- ^2 T7 R' @3 n- S9 c 9
6 i0 s; |% n1 g2 n }9 F 北太平洋板块构造史 4 g' O% s$ ^ C
 fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E) % H, Q: U9 {, @% E) |4 a& F0 L
10
- n* |0 F( B! r A7 Z 南太平洋板块构造史
3 Y% z2 Z! c K/ {0 ~/ Q7 @# V" f  fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E)
3 p5 v2 C( q W; l6 Z/ e3 Z+ Y2 ?3 @ 11
" W- {4 W4 ?; @) X# ^9 {: e 1.7亿年至今,非洲板块和北美洲板块间的大洋中脊的生长过程
2 f3 F( Q, M5 k( N  fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E)
+ l3 b0 E1 G8 w; N! | 12
. G" c# a( L3 @6 D9 J# p+ b. h! h, @ 石油沿断裂和多孔介质向上运移的过程 6 O2 J% x* `$ c7 u
 fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E) : `6 P% v( v8 p
13
4 y& W/ L, w" x- b 圣芭芭拉海峡挤压缩短过程中,油气向上运移和在背斜转折端富集的过程 3 t" F b7 k* a9 O7 i
 fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E)
; Q# J5 r+ e3 q 14 ; @" V7 c2 n8 {
圣芭芭拉海峡南北向褶皱和断裂的形成过程
7 I8 Q- X7 A4 N$ K+ Y( [) X  fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E) % _5 G B/ R1 M* E- g% L$ a) Q
15 9 F7 v" D9 E9 Y
加利福尼亚更新世横断山脉的挤压缩短过程 3 w+ R! n, A$ |2 B. A
 fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E) & m7 m+ I4 q! S
16 - i: v- d, m" `% t1 {) `+ u
加利福尼亚河流冲积平原的形成过程
; k8 N1 B( T0 U& L: `- v  fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E)
* i3 x6 A, g/ Q% ^* Q5 Y+ ` 17 2 p; ^7 K5 p& E# L! J- {$ @- R
加利福尼亚横断山脉演化的过程
9 u& B( F3 ^6 N  fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E)
4 j9 _- v2 b9 Y* V 18
" t) f2 }6 u+ g/ P( p 切萨皮克湾地区,中新世化石层的形成 1 e% f/ f6 N- Q+ p0 k) @
 fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E)
$ G/ {1 r% ]2 d- P9 c( d+ b% c' V 19 & }2 T. L/ K$ k2 x6 d- b" w
切萨皮克湾地区,中新世海岸线移动
3 E- m5 ?1 j% @ (12-16百万年) 4 r# b0 \# ]. I! m! J7 ~9 v) J
 fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E)
干货 | 必修3"区际联系与区域协调发展"。2020-04-05干货 | 高考地理9个易错知识点汇总,学霸们都统统记住了!2020-04-03干货 | 80个高中地理高频考点+80条答题技巧汇总! 干货精选, 超实用!2020-04-01▐ 标签:高考地理 干货整理▐ 更多内容请关注微信公众号平台:高考地理 ID:gkdl100
7 [6 R% O r" w* {1 P ]6 x  fill=%23FFFFFF%3E%3Crect x=249 y=126 width=1 height=1%3E%3C/rect%3E%3C/g%3E%3C/g%3E%3C/svg%3E) 点亮“在看”让更多人看见
9 Q& ~3 d- D3 ?9 B, x( O
& E6 U' d* r+ K& n5 Q! I# |2 T8 K% J0 p0 l/ j2 _# x6 t( l- X' m
/ v7 ^0 ~0 B$ \' A) n$ i3 L4 e, P5 M' ^$ O+ E9 j4 I
|