[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"news-1000000000000000719":3,"session-user":15,"\u002Fapi\u002Fnews\u002Flist?categoryId=1000000000000000024&orderByColumn=publishTime&isAsc=desc&pageSize=5":16},{"id":4,"articleNo":5,"categoryId":6,"categoryName":7,"title":8,"content":9,"publishTime":10,"isTop":11,"isHot":11,"isRecommend":11,"viewCount":12,"collectCount":13,"updateTime":10,"contentHtml":14},"1000000000000000719","760","1000000000000000024","报告资料","原来海洋地质构造如此简单！","![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F0631a6c241ce62b2aa8a228dc9b22d16.gif)**1**\n\n**盘古大陆分裂和大陆漂移**\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fd095be62e65ad1a4d00cd91df649d72f.gif)\n\n**2**\n\n**大陆 - 海洋俯冲带**\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fab5d841acab2110142b60c0a45bdcb70.gif)\n\n**3**\n\n**印度 - 亚洲大陆碰撞**\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fb158a7b02445c7e5d7325d4ba68cc2eb.gif)\n\n**4**\n\n**南大西洋的形成**\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fde04f742bc1b8907ce4d75c1f9ec20b9.gif)\n\n**5**\n\n**海底扩张和海洋磁异常**\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F0631a6c241ce62b2aa8a228dc9b22d16.gif)\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F4d06074216e35694f3e5c0c1a4ae8394.gif)\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fa8ff522a433cd4de2287ffa86f90045f.gif)\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fb156900e1b6cc4b7dda30e80bbe15ad7.gif)\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F7e754d7b2773bc7530f877afe0fcc5ff.gif)\n\n**6**\n\n**加拿大冰盖和海岸线移动**\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fd72b0097327b2387cb5f8d5a3864ea78.gif)\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fe75d7552ea7ec872d266b58aa40bc718.gif)\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F84567f9ab9c98cbb3b9350e3c0cf932a.gif)\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fed4256144530e78d72bf2f4b109bad42.gif)\n\n**7**\n\n**沿海侵蚀与海洋梯田的形成**\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F5cc6a87aa2cdd8adc7f9271f4cb2bcb0.gif)\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F6e78f24b8e7771dae63c94e3cf0af6d6.gif)\n\n8\n\n通过海底扩张形成的南太平洋\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F06fcc398f9b210aba18644ebe44885fe.gif)\n\n9\n\n北太平洋板块构造史\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fc4d0680790a25c0e297c1aa1c4c913e9.gif)\n\n10\n\n南太平洋板块构造史\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F9fa9ef8b129b8e7cf00664a352f111d7.gif)\n\n11\n\n1.7亿年至今，非洲板块和北美洲板块间的大洋中脊的生长过程\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F69b339013d955c1909c0c62aa62cdccc.gif)\n\n12\n\n石油沿断裂和多孔介质向上运移的过程\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fb41b100f0d335a21d21a9f6580fc0128.gif)\n\n13\n\n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\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fd308fc016f10d7f3d16d17fc51140b8b.gif)\n\n14\n\n圣芭芭拉海峡南北向褶皱和断裂的形成过程\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F11c9dc5b54cd2e6962c4781f84bb9415.gif)\n\n15\n\n加利福尼亚更新世横断山脉的挤压缩短过程\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Ff5a86f9b3efa7aabcbb92306fd7d86e0.gif)\n\n16\n\n加利福尼亚河流冲积平原的形成过程\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F69754cabf2c4f70b6678580ad9897b47.gif)\n\n17\n\n加利福尼亚横断山脉演化的过程\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fbc72b05eb45ab2a5bd4f9d2cf1c79407.gif)\n\n18\n\n切萨皮克湾地区，中新世化石层的形成\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Ffca164f2de3f6aac400779a2406776eb.gif)\n\n19\n\n切萨皮克湾地区，中新世海岸线移动\n\n（12-16百万年）\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F04fcc4571aa567594f1c023a3ff9a3ca.gif)\n\n20\n\n加利福尼亚沉积地质类型的形成过程。\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F6d1ecc0ed32e8455988c1831038bc1e4.gif)","2022-03-26T14:07:58+08:00","N",668,0,"\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F0631a6c241ce62b2aa8a228dc9b22d16.gif\" alt=\"\">\u003Cstrong>1\u003C\u002Fstrong>\u003C\u002Fp>\n\u003Cp>\u003Cstrong>盘古大陆分裂和大陆漂移\u003C\u002Fstrong>\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fd095be62e65ad1a4d00cd91df649d72f.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>\u003Cstrong>2\u003C\u002Fstrong>\u003C\u002Fp>\n\u003Cp>\u003Cstrong>大陆 - 海洋俯冲带\u003C\u002Fstrong>\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fab5d841acab2110142b60c0a45bdcb70.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>\u003Cstrong>3\u003C\u002Fstrong>\u003C\u002Fp>\n\u003Cp>\u003Cstrong>印度 - 亚洲大陆碰撞\u003C\u002Fstrong>\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fb158a7b02445c7e5d7325d4ba68cc2eb.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>\u003Cstrong>4\u003C\u002Fstrong>\u003C\u002Fp>\n\u003Cp>\u003Cstrong>南大西洋的形成\u003C\u002Fstrong>\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fde04f742bc1b8907ce4d75c1f9ec20b9.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>\u003Cstrong>5\u003C\u002Fstrong>\u003C\u002Fp>\n\u003Cp>\u003Cstrong>海底扩张和海洋磁异常\u003C\u002Fstrong>\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F0631a6c241ce62b2aa8a228dc9b22d16.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F4d06074216e35694f3e5c0c1a4ae8394.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fa8ff522a433cd4de2287ffa86f90045f.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fb156900e1b6cc4b7dda30e80bbe15ad7.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F7e754d7b2773bc7530f877afe0fcc5ff.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>\u003Cstrong>6\u003C\u002Fstrong>\u003C\u002Fp>\n\u003Cp>\u003Cstrong>加拿大冰盖和海岸线移动\u003C\u002Fstrong>\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fd72b0097327b2387cb5f8d5a3864ea78.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fe75d7552ea7ec872d266b58aa40bc718.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F84567f9ab9c98cbb3b9350e3c0cf932a.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fed4256144530e78d72bf2f4b109bad42.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>\u003Cstrong>7\u003C\u002Fstrong>\u003C\u002Fp>\n\u003Cp>\u003Cstrong>沿海侵蚀与海洋梯田的形成\u003C\u002Fstrong>\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F5cc6a87aa2cdd8adc7f9271f4cb2bcb0.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F6e78f24b8e7771dae63c94e3cf0af6d6.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>8\u003C\u002Fp>\n\u003Cp>通过海底扩张形成的南太平洋\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F06fcc398f9b210aba18644ebe44885fe.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>9\u003C\u002Fp>\n\u003Cp>北太平洋板块构造史\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fc4d0680790a25c0e297c1aa1c4c913e9.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>10\u003C\u002Fp>\n\u003Cp>南太平洋板块构造史\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F9fa9ef8b129b8e7cf00664a352f111d7.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>11\u003C\u002Fp>\n\u003Cp>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\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F69b339013d955c1909c0c62aa62cdccc.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>12\u003C\u002Fp>\n\u003Cp>石油沿断裂和多孔介质向上运移的过程\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fb41b100f0d335a21d21a9f6580fc0128.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>13\u003C\u002Fp>\n\u003Cp>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\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fd308fc016f10d7f3d16d17fc51140b8b.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>14\u003C\u002Fp>\n\u003Cp>圣芭芭拉海峡南北向褶皱和断裂的形成过程\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F11c9dc5b54cd2e6962c4781f84bb9415.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>15\u003C\u002Fp>\n\u003Cp>加利福尼亚更新世横断山脉的挤压缩短过程\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Ff5a86f9b3efa7aabcbb92306fd7d86e0.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>16\u003C\u002Fp>\n\u003Cp>加利福尼亚河流冲积平原的形成过程\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F69754cabf2c4f70b6678580ad9897b47.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>17\u003C\u002Fp>\n\u003Cp>加利福尼亚横断山脉演化的过程\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Fbc72b05eb45ab2a5bd4f9d2cf1c79407.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>18\u003C\u002Fp>\n\u003Cp>切萨皮克湾地区，中新世化石层的形成\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002Ffca164f2de3f6aac400779a2406776eb.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>19\u003C\u002Fp>\n\u003Cp>切萨皮克湾地区，中新世海岸线移动\u003C\u002Fp>\n\u003Cp>（12-16百万年）\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F04fcc4571aa567594f1c023a3ff9a3ca.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>20\u003C\u002Fp>\n\u003Cp>加利福尼亚沉积地质类型的形成过程。\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20220326\u002F6d1ecc0ed32e8455988c1831038bc1e4.gif\" alt=\"\">\u003C\u002Fp>\n",null,{"items":17,"total":49,"pageNum":50,"pageSize":51},[18,24,30,37,43],{"id":19,"articleNo":20,"categoryId":6,"categoryName":7,"title":21,"publishTime":22,"isTop":11,"isHot":11,"isRecommend":11,"viewCount":23,"collectCount":13,"updateTime":22},"1000000000000001141","74385","一图读懂 | 中国持久性有机污染物控制（2004-2024年）","2024-05-18T23:03:36+08:00",1421,{"id":25,"articleNo":26,"categoryId":6,"categoryName":7,"title":27,"publishTime":28,"isTop":11,"isHot":11,"isRecommend":11,"viewCount":29,"collectCount":13,"updateTime":28},"1000000000000001138","74382","专家解读 | 深入打好净土保卫战的新阶段","2024-05-09T16:28:47+08:00",1101,{"id":31,"articleNo":32,"categoryId":6,"categoryName":7,"title":33,"publishTime":34,"isTop":11,"isHot":11,"isRecommend":11,"viewCount":35,"collectCount":13,"updateTime":36},"1000000000000001128","74372","生态环境部召开生态环境监测工作会议","2024-04-13T23:23:53+08:00",1431,"2024-04-22T20:19:06+08:00",{"id":38,"articleNo":39,"categoryId":6,"categoryName":7,"title":40,"publishTime":41,"isTop":11,"isHot":11,"isRecommend":11,"viewCount":42,"collectCount":13,"updateTime":41},"1000000000000001125","74369","土壤污染状况调查之采样方案的上传","2024-04-12T21:15:55+08:00",1801,{"id":44,"articleNo":45,"categoryId":6,"categoryName":7,"title":46,"publishTime":47,"isTop":11,"isHot":11,"isRecommend":11,"viewCount":48,"collectCount":13,"updateTime":47},"1000000000000001123","74367","使用surfer绘制地下水流场图","2024-04-12T19:53:44+08:00",6813,137,1,5]